~ppendices

~ppendix 1 Tectonic Dataabout Archaen andPaleoproterozoic

Vtppendix 1.1 Rock formation time, temperature, pressure, depth and geothermal Igradient in Archaen

Isotopic Tempera- Pressure Formation Geothermal Area Lithofacies Sources age (Ma) ture ('C) (GPa) depth (km) gradient ('Clkm) Qingyuan, Liaoji granulite 2,924 800 1.0 36.7 18.3 Shen BF et aI., continental nucleus 1994 Anshan, Liaoji granulite > 2,900 800 1.1 36.7 18.3 Cheng YQ et aI., continental nucleus 1994

~J' e- , "'. ., continental nucleus 1992 South of Chifeng granulite 2,846 990 1.1 36.7 23.4 CuiWY et aI., continental nucleus 1991 Jining, Dongsheng granulite > 2,900 860 I 36 20.3 Cheng YQ et aI., continental nucleus 1994 Qiari'an, Bohai amphibolite 3,561 900 1 33 23.3 ShenQH et aI., continental nucleus 1992 Xishui, Bohai granulite > 2,900 800 0.75 25 26.8 Cheng YQ etal., continental nucleus 1994 Gongdanshan, Yishui, granulite > 3,000 900 0.95 1.7 24.3 Su SG et aI., 1997 Shandong Qianxi, Bohai granulite 3,300 800 1.2 40 16.8 Dong SB et aI., continental nucleus 1986 Linfen continental granulite > 2,800 900 1 33 23.3 Wu JS et aI., 1989 nucleus Jining continental amphibolite 2,788 600 0.6 20 23.5 Xu HF et aI., nucleus 1992 Above 11 areas Average MA 827 0.95 32 22.2 Qingyuan, Jiliao amphibolite 2,624 610 0.61 20 25.5 ShenQH et aI., continental nucleus 1992 Jiapigou, Jiliao amphibolite 2,525 600 0.6 20 25 Shen QH et aI., continent nucleus 1992 1386 Appendlcesl

Isotopic Tempera- Pressure Formation Geothermal Area Lithofacies Sources age (Ma) ture ("C) (GPa) depth (km) gradient "Clkm Huadian, Jiliao granulite ~ 2,500 830 0.6-1 30 24.3 Bureau of Geol- continental nucleus ogy of Jilin, 1988 Tonghua, JiHao granulite ~ 2,560 750 0.62 27 24 continental nucleus Qingyuan, Jiliao granulite ~ 2,630 1000 0.75 33 27.3 Cheng YQ et aI., continent nucleus 1994 Anshan, Jiliao greenschist ~ 2,630 570 0.6 20 23.5 Cheng YQ et aI., continent nucleus 1994

caM VI rUMlUIl, -",to' JlV l.V JJ t z., LlIl lA er ar., Liaoning boleschist 1995 Jiapigou, Jilin granulite > 2,500 850 1.3 43 17.4 SunXM et aI.,1992 Chongli, Chifcnz amphibolite 2,470 730 0.91 30 21 Chen QA et aI., continent nucleus 1992 Pingquan, Chifeng granulite 2,650 790 0.8 26.7 25.8 Tan YJ et aI., continental nucleus 1991 Pingquan, Chifeng amphibolite 2,505 670 0.7 23 24.8 Tan YJ et aI., ,n,

Chongli, Chifeng granulite 2,454 868 0.9 33 23.3 WangRM et aI., continental nucleus 1994 West Liaoning, granulite 2,494 8oo I 40 17.5 Dong SB et aI., Chifeng nucleus 1986 West Liaoning granulite 2,575 860 1.25 41.7 18.2 JiJQ et aI., 1998 Jianping, West granulite 2,490 820 1.17 39 18.5 Wei CJ etal., Liaoning 2oo1 Jianping, West granulite 2,487 850 1.05 35 21.4 WangCQ Liaoning et aI.,1999 Jianping, West granulite 2,575 860 1.25 42 20.6 Ji JQ et aI., 1998 Liaoning Ruanping, Chengde, granulite > 2,500 8oo 1.20 40 17.5 Li JR, 1998 North Hebei Huai'an, Northwest granulite > 2,600 860 0.92 31 24.5 Geng YS et aI., Hebei 2oo0 Sanggan area, North- granulite 2,530 830 1.25 42 17.4 GuoJR et aI., west Hebei 1998 Dongsheng amphibolite 2,625 880 0.8 26.7 33 Jin Wet a!., 1991 continental nucleus Wulashan, Dongsheng granulite ~ 2,500 710 0.84 28 21.8 Cheng YQ et aI., continental nucleus 1994 Daqingshan, Dongsh- greenschist ~ 2,550 5oo 0.4 13.3 30 Cheng YQ eng continent nucleus et al.,l994 Bohai continent amphibolite 2,663 680 0.5 16.7 34.7 Shen QH et aI., nucleus 1992 Miyun, Bohai granulite 2,523 9oo 1 36 22.2 Dong SB continental nucleus et al.,l986 Miyun, Beijing granulite > 2,500 9oo 1.02 34 23.5 He GP et aI., 1994. Zunhua, Qian'an, granulite > 2,500 920 1.14 38 21.6 Chen MY et aI., East Hebei 1996 f'\ppendix I Tectonic Data about Archaen and Paleoproterozoic 3871

Isotopic Tempera- Pressure Formation Geothermal Area Lithofacies Sources age (Ma) ture ('C) (GPa) depth (km) gradient I'C/km) Qianxi group, granulite < 2,700 940 1.1 37 22.7 He GP et aI., 1992 rz. r.r. Jiaodong, Bohai granulite ~ 2,800 700 0.65 20-23 27.9 Yang ZF et aI., continental nucleus 1998 Jiaodong Group, amphibolite ~ 2,500 655 0.65 20-23 25.8 Yang ZF et aI., Bohai nucleus 1998 Linfen nucleus amphibolite > 2,500 670 0.8 26.7 21.3 Wu JS et aI., 1989 Wutai, Linfen amphibolite ~ 2,550 690 0.8 26.7 22 Cheng YQ et aI., continental nucleus 1994 Yanggao, Linfen granulite 2,440 900 1.4 41 19.5 Dong SB et aI., '00£

Dengfeng, Linfen amphibolite ~ 2,500 450 0.35 11.7 30 Cheng YQ et aI., continental nucleus 1994 Luonan, Linfen granulite ~ 2,500 650 0,6 20 27.5 Cheng YQ et al., continental nucleus 1994 Wutai-Taihang area gneiss > 2,500 700 0,6 13-20 36.4 WangKY et aI., 1991 Taihangshan rich alumi- > 2,600 800 0.8 26.7 26.2 LiuSW et aI., niumgneiss 1997 ., nucleus Taishan, Jining granulite > 2,626 700 I 33 18.2 Bureau of Geo- continental nucleus logy of Shandong, 1991 Taishan, Jining amphibolite > 2,626 660 0,8 26.7 21 continental nucleus Huoqiu, Jining amphibolite 2,681 600 0,5 20 25 Dong SB et aI., continental nucleus 1986 North lone eo,' 7 hllll h()() 117 7, , 0; TV 7 " Qinling 1992 Huabei eclogite < 2,500 900 1.2 40 20 Zhai MG etal., 1995 Jiamusi continental amphibolite 2,539 690 0.55 18.3 32.2 Cheng YQ et aI., nue eus I~~'t Helanshan, Alaxa granulite ~ 2,500 800 0.65 21.7 32.2 Cheng YQ et aI., 1994 Middle Kangdian amphibolite > 2,400 600 0.41 14 35.7 LuMJ, greenstone belt 1986 South of Kangdian greenschist > 2,400 550 0.53 17.7 25.4 LuMJ, greenstone belt 1986 Above 47 areas Average NA 714 0.81 27.5 24.2 World (average) granulite Arch. >750 0.41 14 54 Grambling, 1981 1388 Appendices

Vtppendix 1.2 Blockmotion velocity in the Chinese continent ofArchean (3.2-2.5] IGtiJ

~rea Rock Sampleamount Isotopicage (Ga) Deformationvelocity(cm/yr] Xm'antun, Jtlm gramtOld 8 3.2- 2.8 5.2 ~nshan, Liaoning harzburgite 4 > 2.5 -0.88 Raobazhai, Anhui ultrabasicrock 29 about 2.8 - 2.7 -0.87 Wutaishan,Shanxi basic lava 80 about 2.8 - 2.7 -0.72 ~Ihong, Jlangsu ultrabaslcrock 2 about 2.8 2.7 0.8~ Wutaishan,Shanxi basic lava 79 about 2.7 - 2.6 -0.67 Luliangshan,Shanxi basic lava 25 about 2.7 - 2.6 -0.8~ IIonghua, Jlhn dlOntOld 2 about 2.8 - 2.5 4~ IWutaIshan, ShanxI aCidIc lava 4 about 2.7 - 2.6 5.) North of Altun basIclava 2 2.46 0.78 North of Altun acidicJava 4 250 54 Luliangshan, Shanxi basic lava 12 about 2.6 - 2.5 -0.56 IZhongtIaoshan, ShanXI baSIC lava 11 about 2.6 2.5 0.48 Jilin granitoid 8 about 2.6 - 2.5 5.4 Baotcu, Inner Mongolia granitoid 2 about 2.6 - 2.5 5.~ [iihangshan, ShanXI aCidIc lava 27 about 2.6 - 2.5 4.2 IZhongtmoshan, ShanXI aCidIc lava 15 about 2.6 2.5 5.~ IWutaIshan, ShanXI gramtOld 86 about 2.8 2.5 5.] [Iaishan, Yishan,Shandong granitoid 10 about 2.8 - 2.5 4.87 [Iaishan, Zouxian,Shandong granodiorite 6 about 2.8 - 2.5 4.~ Bengbu,Anhm gramtOld about 2.6 - 2.5 4.1

Note:" "IS extensIOn velocIty, othersare shortemngvelOCltIesJ [he rock chemicaldata got from I:200,000regional geologicalsurveyreports in those areas and regionalgeology abou~ ~hose provinces.

Vtppendix 1.3 Rockformation age,temperature, pressure, depth andgeothermal Igradient in Paleoproterozoicl

Isotopic Tempera- Pressure Formation Geothermal Area Lithofacies Sources age (Ma) ture ("e) (GPa) depth gradient I(km) ("e/km) East of Hingganling, amphibolite ~ 1,900 625 0.25 8.3 66.9 Cheng YQ et aI., 1994 Heilongjiang MashanGroup, gneiss > 1,900 850 0.47 15.7 49.7 Jiang JS et al., 1993 Heilongjiang East of Liaoning- amphibolite ~ 1920 660 0.8 26.7 22.1 Cheng YQ et al., 1994 South of Jilin Liaohe Group, amphibolite > 1,900 630 0.8 26.7 20.1 Li SZ et al., 2001 NorthLiaoning Liaohe Group, amphibolite > 1,900 600 0.7 23 23 Li SZ et al., 200I Q •••• East of Liaoning- low grade < 1,900 640 0.73 24.3 23.5 He GP et al., 1998 Southof Jilin amphibolite Jianping,Westof granulite 2,490 820 1.17 39 19.2 WeiCJ et al., 2001 Liaoning f'\ppendix I Tectonic Data about Archaen and Paleoproterozoic 38~

Isotopic Tempera- Pressure Formation Geothermal Area Lithofacies Sources age (Ma) ture (OC) (GPa) depth gradient Ilkm\ rOC/km\ Shuangshanzi, amphibolite 2,193 548 0.63 20-25 21.2 Dong SB et al., 1986 East Hebei Xinghe, Inner granulite ~ 1,900 850 I 33 23.6 Mei HL et al., 1998 Mengolia

, UH"UA' . ""'" .lVV " , .U m5u~ "'-, Wutaishan, Shanxi greenschist ~2,129 400 0.33 11 30 Dong SB et al., 1986 Shanxi-Inner kbondalite 1,800 750 0.6 20 34 Wu CH et al., 1997 Mongolia Haivanssuo I zranufite > 1900 1050 1.24 41 23.9 Su SG et a1. 1996 Jiaodong, Shandong Gejiaji, Jiaodong, granulite > 1,900 700 0.9 30 21 Su SG et al., 1996 Shandong Jingshan, Jiaodong, amphibolite ~ 1,800 600 0.45 16.7 31.7 Yang ZF et al., 1998 ..>Uauuvu,; Jiaodong-Laixi- gneiss < 1,900 750 0.7 23.3 29.2 Lu LZ et aI., 1998. Laiyang Jiaonan Group, eclogite > 1,901 810 1.2 40 18.5 Bnrean of Geology of Shandong Shandong, 1991 Jiaonan Group, amphibolite > 1,901 580 0.65 21.7 23.5 Shandong Songshan, Henan greenschist ~2,071 400 0.2 6.7 49.5 Cheng YQeta1., 1994 Beishan, Gansu amphibolite 2,150 620 0.55 18.3 30 Cheng YQ et a1., 1994 Dunhuang, Gansu amphibolite ~ 1,900 660 0.55 17 -20 31.9 Gansu Geology Bu- reau, 1989 Qilianshan amphibolite 2,205 540 0.5 16.7 28.1 Cheng YQ et al., 1994 Mid-Qilianshan amphibolite 2,205 900 0.9 30 27.7 Qinghai Geology Bu- n;nah"; rp"" 1001 Northern Qaidam amphibolite > 1,900 800 0.9 30 24.3 Southeastern Qaidam amphibolite 1,846 800 0.85 28 26 Middle part in south amphibolite 1,846 750 0.75 25 27.2 margin of Qaidam West part in south amphibolite 1,846 700 0.4 13.3 47 margin of Caidarn Badu, Zhejiang amphibolite ~ 1,900 680 0.7 23.3 26.2 Cheng YQ et a1., 1994 Maoji, Tongbaishan granulite > 1,967 650 0.8 17 -27 26.4 Liu GH et al., 1993

lJaU10,lIaU, r-ieuau ,~o~ , iJ v. LJ.J "to.J UiOU~ L", 0' eu., i ~~' Luotian-Huilan, granulite > 1,900 880 1.29 43 18.8 You ZD et al., 1995 Dabieshan Ailaoshan Group, amphibolite ~ 1,900 650 0.49 16.3 35.6 Zhong DL, 1998 Yunnan Dahongshan, Yunnan hornblende > 1,900 533 0.94 31 15 Qin OX et al., 2000 Diancangshan Group, amphibolite ~ 1,900 780 0.82 27.3 26 Zhong DL, 1998 Yunnan Average of 28 areas amphibolite 681 0.78 28.5 24.6 1390 Appendices Vtppendix 1.4 Deformation velocity in continental plateDuringLiiliangperiod 1(2.5-1.8 Ga), Paleoproterozoiq

Area Rock Sampleamount Age(Ga) f1uma,Shuangyashan, gabbro 4 2.5 2.4 f1ellongjtang [Iaihang, Luliang,Shanxi basalt 36 2.5-2.4 -0.551 rhaoyanggou, Llaomng gabbro 2 2.5 2.4 0.751 ~W Jllantm, InnerMongolta gabbro 2 2.5- 2.4 -0.651 [Imhang, Ltiltang, ShanxI basalt 57 2.5- 2.4 -0.451 Jlaobel, Shandong ultrabaslc-baslc 55 2.5 2.4 0.81 [Iaipingxi, Hubei ultrabasic-basic 25 2.5- 2.4 -0.81 rangshan, Yunnan ultrabaslc-baslc 2 2.5 2.4 0.71 k\I1aoshan, Yunnan ultrabaslc-baslc 2 2.5 2.4 II Liaoning intermediate-basic rock 6 > 1,900 5.61 Westof Shandong granodIOrIte 20 2.075- 1.754 4.61 Westof Shandong metamorphIc gabbro 8 2.075- 1.754 6 [Imhang, ShanxI gramtOld 67 2.5 2.4 5.~ QI1lanshan-Belshan, Gansu daCIte 2 2.5 2.4 5.~ [Iongshan-Pixian, Jiangsu ultrabasic rock 1 2.0-1.8 -0.'1 rangshan Group,Yunnan basIcvolcamcrock 2 ~ 1.9 0.71 k\ilaoshan Group,Yunnan basicvolcanic rock 3 ~ 1.9 -0.81 ~apeiquan, Altun basicvolcanic rock 13 ~ 1.793 -0.5 ~apelquan, Altun slhcIC volcamc rock 5 ~ 1.793 8.~ Erguna,Jiamusi, Yichun granitoid 30 2.0- 1.8,1.705 4.71 ~udargan, Mayatu, InnerMongolIa granItOId 3 2.0 1.8 6 Mlaohe,JI1lao activebelt granItOId 5 2.0 1.8 5.81 NorthHebei- Liaoningactivebelt granitoid 1 2.0-1.8 5.81 fost-tectomc stage, North Hebel- gramtOld 2.0-1.8 4.81 Liaoningactivebelt Jilin granitoid 2 1.955- 1.781 5.81 Wutmshan, ShanxI granItOId I 2.0 1.8 M [Iaihangshan, Shanxi granitoid 2 2.0-1.8 5.91 puandishan,Ltiliangshan granitoid 1 2.0-1.8 5.61 pableshan, Henan gramtOld 16 2.005 6.(J Middlepartof Helanshan granitoid 16 1.84 7.11 Huoyanshan, Gansu granitoid 16 2.0-1.8 4.91 IKuruktag granItOId 22 1.9 1.8 6.91 ~ast of Kunlun gramtOld 5 1.9-1.8 6.~ [iantangzhai, Hubei granitoid 14 2.0-1.8 5.81 Jiaonan, Shandong gramtOld 11 2.0-1.8 6.~ Donghai xian,Jiangsu meta.volcanite 1 2.0-1.8 5.11 Jlangsu granItOId 10 1.928 5.71 ~ote:" , IS extension velOCIty, othersare shortemng velocltles.1 ~ock chemical dataarequotedformthereportof I:200,000regIOnal geological survey III theseareasand regIOnal geologYI ~11 pluvIIlces.1 f'\ppendix I Tectonic DataaboutArchaenand Paleoproterozoic 391

Vtppendix 1.5 Estimated thickness for Archean-Paleoproterozoic continental crustl ~n Chinese platel

Location Geological age Rock (km) IQianxi, Hebei 3800Ma chamockite 1 1.02 19.01 IQIanxI, Hebel Paleo-& Meso-Archean tonahte I 1.05 19.5(J IQlan' an, Hebel Paleo-& Meso-Archean tonahte 9 2.17 39.9 k\nshanGroup Neoarchean amphlbohte I 1.13 21 Molijiang,Liaoning Neoarchean plagiogranite 1 1.07 19.9 IWutar, ShlZUl Neoarchean amphlbohte 13 0.8 15.081 IWutarshan, ShanxI Early of Neoarchean meta. basalt 77 0.99 18.51 ~utaishan, Shanxi Middleof Neoarchean meta.basalt 45 0.84 15.~ ILiihangshan Late of Neoarchean meta. basalt 37 1049 27.6 IWulashan Group Neoarchean plagiogneiss 1 1.62 29.93 ICularshan, Shandong Neoarchean epldlOnte 24 1.66 30.6 "'orth of Arjmshan Neoarchean plaglOgnelss 2 0.76 14.281 Cangshan,Yunnan Neoarchean meta.basalt 2 0.88 16.~ IAilaoshan, Yunnan Neoarchean meta.basalt 2 0.43 8.3 IAbove areas Neoarchean basic rock 205 21 51 [lantazi Group Neoarchean plagiogranite 2.98 54.6~ IE Anshan,Liaoning Neoarchean trondhjemite I 3.54 64.9 Lishan,Liaoning Neoarchean trondhjemite 1 3.4 6~ IChentargou, Llaomng Neoarchean trondhjemite I 3.59 65.~ [Iiejiashan, Liaoning Neoarchean granitoid 1 4.98 91.1 IXin'antun, jilin Neoarchean granitoid 8 3.39 62.2 [larshan, Shandong Neoarchean mlgmatlte 31 2.81 51.55 IShlgujIan, Anhul Neoarchean epldlOnte 2 3.5 64.15 INorth Altun Neoarchean gramtegneiss 4 4.25 77.~ IAbove areas Neoarchean granitoid 50 66.0~ Nauonal average Archean (ChengYG, 52 3.54 64.8~ If994) IHuma, HeIlongjiang PaleoproterozOic meta.gabbro 10 1.6 29.6 paoli Duntai,Liaoning Paleoproterozoic monzonitic 1 1.1 20.~ gramte Ilonghua, Jlhn PaleoproterozOic dlOnte 2 1.7 31.4 ~ilantai, InnerMongolia Paleoproterozoic meta.gabbro 2 1.21 22.~ [Iaihangshan, Liiliang, Shanxi Early stage of Paleopro- meta.basalt 57 1.78 32.~ IterozOic [laoke,Shandong PaleoproterozOic meta.gabbro 24 1.79 32.95 IKuruktag PaleoproterozOic amphlbohte 5 1.74 32.11 IKuruktag PaleoproterozOic plaglOgramte 7 2.05 37,] North Altunshan Paleoproterozoic granodiorite 9 2.02 37.2 ~ast Kunlunshan PaleoproterozOic quartzdlOnte 5 104 25.9 IQlhan, Gansu PaleoproterozOic meta.daCIte I 1.6 29.6 IAbove areas PaleoproterozOic inter, baSIC rock 123 30.2 IBelshan, Gansu PaleoproterozOic meta.daCIte 1 2.9 53.2 Huoyanshan, Gansu Late ofPP granitoid 16 4.13 75·1 paohduntar, Llaomng Late ofPP gramtOid 5 2.5 4(J IHuaplgou, HeIlongjIang Late of PP gramtOid 30 2043 44.~ !De'er, longte, InnerMongoha Late of PP gramtOid 4 2.27 41.1 1392 Appendices

Contmued

Location Geological age Rock

IWestKunlunshan Paleoproterozoic guartz diorite [Iaihang, Liiliang Late ofPP granitoid rlaoke, Shandong PaleoproterozOic quartz dlOnte 20 2.91 Zouxian, Shandong Paleoproterozoic granodiorite II 2.87 IKuluketag PaleoproterozOic mlgmatIte 3 2.87 ~Aaohe Group PaleoproterozOic leptIte 1 4.16 IAboveareas Paleoproterozoic granitoid 180 !"atlOnal average PaleoproterozOic (Cheng YQ, 361 3.4 62.33 ll2W !"ote: ChemIcal analysIS data were guoted from Cheng YQ (1994) and geology of provmces (1984=1993).

IReferences for Appendix ~

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Liu YX, Sun DY, Liu PJ (1995) The upper Archean enslavement of magnesioriebechites-bearing gneiss in Liaoning! provmce: Old glaucophane-schist reltct.Acta PetrologlcaSmlca 11(1):83 92 (m Chmesewith Engltshabstract). ,"u LZ, Dong YS(1998) Ihe P-I-X phaserelatIOns and theIrevolutIOn for the eqUlltbnum assemblages of AI-nch gnelssesl from Early ProterozoIc hngshan Group m east Shandong. Acta Petrologlca SlnIca 14(2): 140=151 (m Chmese wlthl Englishabstract). ,"u MJ (1986) Early Proterozoic metamorphic rock senes, west Sichuan and east Yunnan, Chma. Journal of Changchunl Collegeof Geology45(3): 12-22 (in Chinesewith Englishabstract). Mei HL, Yu HF, Li Q et al (1998) The first discoveryof eclogite and Paleoproterozoic granitoids in the Beishan area, northwestern GansuProvince,China.ChineseScienceBulletin44(4): 356-3611 RI IY (1992) Metamorphicrock senes of huhua Group and conditIOns for Its formatIOn m eastern Qmgltng. SClentIal GeologicaSimca (suppl.):94=107(m Chmesewith Engltsh abstract)j Qin OX, YanYF,TianYL et al (2000)Geologicalcharacteristics andore-formingevolutionof Dahongshancopperdeposit. ScientiaGeologicaSinica 35(2): 129-139 (in Chinese withEnglish abstractj] IShen BF,Luo H, Han GG et al (1994) Archean Geologyand MetalltzatIonm NorthernLIaonmgProvmce and Southerij hIm Provmce.GeologicalPubltshmgHouse,Beljmg(m ChmesewIthEngltshabstract)j IShen QH, Xu HF, Zhang ZQ et al (1992) Early PrecambrianGranulites of China. 237pp. GeologicalPublishingHouse, Beijing(in Chinese). ISu SG,Lai XY,ZhangCL (1996)P-Tevolution of granulitesand their petrogenetic significance in Haiyangsuo andGejiajj areas, Jiaodong.Geosciences10(4):455-460 (in Chinese withEnglish abstracnl ISu SG, Gu DL, Zhu GX (1997) Ihe P-I diagram and Its tectOnIC signIficance of granultte facies metamorphism m th~ YIShUl area, ShandongProvmce.Acta PetrologlcaSmlca 13(3):331 345 (in Chmesewith Engltshabstract).1 ISun XM, Xu KQ, Ren QI et al (1992) ConfirmatIOn of the lraplgou Archaean high grade metamorphic terram and It§ geologicalsignIficance. ChmeseSCience Bulletm 37(10):847 850. [fan YJ, WangGC, Li SX (1991) ArchaeanGeologyand Its Constraintsto Gold Prospectingin Pingquan-Chengde Area, NorthHebei Province.80pp.ChinaUniversityof GeosciencesPress, Wuhan(in Chinesewith English abstractj] ~ang CQ, Cui WY,Kroner A et al (2000) Zircon isotopic ages from magnetitequartzites of the Jianping metarnorphid complex,westernLiaoningProvince.Chinese ScienceBulletin45(6): 547-551J IWang KY,LI IL, Lm RQ (1991) Ongm of the Fupmggneisses.SClentIa GeologicaSmlca (3): 254=267 (m Chmese wlthl Engltshabstract). IWang RM, Lai XY,Dong WDet al (1994)Some proof of Neoarcheancollisionalbelt in northwestern HebeiProvince.In: Qian XL,WangRM (eds)GeologicalEvolutionof GranuliteBelt in NorthPart of NorthChina.pp.7-20.Seismologica] Press, Beijing (in Chinese). ~ei CJ, Zhang CG, Zhang AL et al (2001) Metamorphic P-T conditions and geological significance of high-pressure granulite from the Jianpingcomplex, westernLiaoningProvince. Acta PetrologicaSinica 17(2):269-282 (in Chines~ withEngltsh abstract). IWu CH, Zhong CI, Chen QA (1997) DISCUSSIOn on the age of khondalttem lm-Meng (ShanxI-Nel Mongol) high gradij terrain. Acta PetrologicaSinica 13(3):289-302 (in Chinesewith English abstract). ~u JS, GengYS,Xu HF (1989)Metamorphicgeologyof FupingGroup.JournalofInstitute of Geology,ChineseAcademyi of GeologicalSciences,(19): 2l3~ p(uHF,Dong YJ, Shi YH et al (1992)Granite-Greenstone Belt in WestShandongProvince.84pp. GeologicalPublishing! House,Beljmg(m Chmese).1 IYang ZF et al (1998) Ihe EvolutIonof RegIOnal Crust and the Geochemistry on Gold MmeraltzatlOn m llaodong. 157pp. GeologicalPubltshmgHouse,Bellmg(m ChmesewIthEngltshabstract). IYou ZD, Chen NS, ChristopherIC (1995) Ihe metamorphism of deeper crust m the Dable Mountams:as eVidenced b5J the study of granulites near Huilanshan, Luotian. Acta Petrologica Sinica 11(2): 137-147(in Chinese with Englishl abstract).1 Zhai MG, Guo JH, Li JH et al (1995)Discoverythe retrogressive metamorphic eclogitein Archeanof NorthChinaand it~ significance. ChineseScienceBulletin40(17): 1590-15941 ghong DL (1998) PaIeo-Iethyan OrogenIcBelt m Western Yunnan and Sichuan. 231pp. SCience Press, Beljmg (m ChIj nese)J 1394 Appendices k\ppendix 2 Thickness andForming Velocity of Sedimentary Strataof Chinese Continenti

IIhlckness of sedimentary rocks(m) Formmg veIoclety of strata(ril7Myr) No Area Meso- & Paleo- Meso- Ceno- Tolal Meso- & Paleo- Meso- Ceno- I Neoprol. zoic zoic zoic thickness Neoprol. zoic zoic zoic 11 Hmgganhng, Heilongjiang 10,692 21,508 22,479 3,158 57,832 8.5 73.4 121.5 48.51 2 JlamUSI, HeilongJIang 6,357 20,609 20,286 696 47,948 0.2 70.3 109.6 10.1 3 Yanhian, Jilin 22,043 16,805 2,996 41,844 75.2 91 46 4 Hingganling, Inner 2,064 22,319 10,249 520 35,152 1.6 76.2 55.4 ~ ~ 5 Ymshan, InnerMongoha 1,281 3,721 13,573 4,957 23,532 9.4 12.7 73.4 76] 6 Belshan, InnerMongoha 8,880 27,189 4,300 731 41,100 7.1 92.8 23.2 Il.21 7 Altay-Junggar 9,241 41,110 6,770 4,224 61,345 7.4 140.3 36.6 65 8 Tianshan 7,195 23,743 5,454 3,635 40,029 5.7 81 29.5 56 9 Southeast Jilin 19,053 4,237 10,700 1,786 35,776 15.2 14.5 58 27.51 10 EastLiaoning 4,214 5,006 8,660 2,009 19,889 3.4 17.1 47 31 11 WestLiaoning 11,718 2,285 13,891 5,453 33,347 9.3 7.8 75 83.~ 12 Yanshan 9,200 1,733 35,435 125 46,333 7.3 3.7 191.5 9.6 13 'Imhangshan 3,126 2,210 2,766 1,130 9,232 2.5 7.5 15 17.41 14 Plmnof Heibel 2,183 2,266 2,766 13,000 20,215 1.7 7.7 15 20q 15 EastShandong 1,200 1,349 4,781 2,619 9,949 2.6 4.6 25.8 40 16 WestShandong 4,103 3,640 1,733 9,476 14 20 27 17 NorthHenan 19,206 2,452 6,152 4,607 32,417 15.3 8.4 33.3 70.~ 18 NorthAnhui 4,285 3,559 7,377 1,111 16,332 9.4 12 39.9 17 19 NorthJlangsu 5,207 1,597 3,326 1,889 12,306 11.7 5.9 18 29 I(m Smo-Korean-P1ate) 20 Northeast ShanXI 1,342 1,007 6,052 1,224 9,625 1.1 3.4 33 19 21 Southeast ShanXI 6,789 1,255 2,563 3,777 14,384 5.4 4.3 14 58 22 WestShanxi 875 874 4,055 183 5,987 0.7 3 22 2.8 23 Erdos 14,156 944 5,405 543 21,048 11.3 3.2 29.2 8,4 24 EastNingxia (Qingyang) 1,571 2,573 3,975 2,899 11,018 1.2 9 21.5 44.§ 25 Dable,Hubel 27,719 3,619 800 2,922 35,060 22.1 12.3 4 45 26 EastQmhng 18,124 11,394 9,721 3,363 42,602 14.4 38.9 52.5 5q 27 Qmhng-Wudang, Hubel 11,487 12,950 800 2,469 27,706 9.1 44.2 4 38 28 MiddleQinling 23,592 15,152 8,224 1,051 48,019 37 51.7 44.5 16.21 29 WestQinling, Gansu 26,284 18,507 8,087 2,155 55,033 20.9 63.2 43.7 33.21 SO Jiangsu (in Yangtze plate) 1,763 8,893 8,436 7,461 26,553 3.9 30.3 45.6 114.8 31 SouthAnhui 4,785 7,019 20,093 2,000 20,543 10.5 23.9 109 30.~ P2 Northwest Zhejlang 1,235 9,311 11,410 1,771 24,056 4.8 24.2 61.7 32] P3 NorthJlangxl 22,778 10,556 10,165 1,879 45,378 18 36 54.9 28.~ [34 SouthHubel 639 4,524 11,873 1,015 18,051 3.1 15.4 64.2 15·G 135 NorthandMiddleHunan 774 4,544 7,928 1,264 14,510 3 15.5 43 19.41 P6 MiddleGuangxI 6,577 3,861 764 11,202 22.5 21 11.~ P7 Southeast GuangxI 42,755 33,342 6,315 82,412 146 180.2 97.21 P8 NorthGuangxI 16,261 16,261 12.9 I 139 Dabashan, Sichuan 10,490 3,402 3,876 4,035 21,803 8.3 11.6 21 62 ~O Chengdu-Xichang 14,436 7,838 10,710 2,332 35,216 56.2 27 58 35.~ ~1 Chongqing-Chengkou 1,802 4,330 5,600 265 11,997 7 14.8 30 4.11 ~2 Midd1e& West Guizhou 4,607 9,842 6,248 1,016 21,760 7.4 33.6 33.8 15.(1 43 Southeast Gmzhou 4,223 4,000 150 8,373 14.4 21.6 2.3 44 Kunmmg 1,454 8,664 11,071 1,548 22,737 5.7 29.6 59.8 24 45 Southeast Yunnan 5,U92 11.177 12,225 1,508 30,002 19.8 38 66 23 ~6 Southeast Zhejiang > 3,000 12,220 378 15,598 11.7 66.1 5.8 ~7 EastFujian 13,453 3,523 5,410 857 23,243 29,4 12 29 13 ~8 WestFujian 18,929 11,078 18,636 315 39,789 37 37.8 101 4.8 ~9 EastTaiwan 7,350 7,350 1131 50 West Imwan 14,610 14,610 224.8 51 SouthJlangxl 6,428 17,050 22,389 1,320 40,759 14 58 121 20.~ 52 Southeast Hunan 4,277 13,082 7,004 920 25,283 16.6 44.6 38 14.21 ~ppendlX 2 rhlcknessandFormmg VeloCity of Sedimentary Strataof ChmeseContment 395

IContmuedl IIhlckness of sedimentary rocks(m) Formmgveloclety of strata(ril7Myr) No Area Meso- & Paleo- Meso- Ceno- Total Meso- & Paleo- Meso- Ceno- I Neoprot. zoic zoic zoic thickness Neoprot. zoic zoic zoic 53 West & NorthGuangdong 5,501 17,433 7,142 1,553 31,629 21.4 59.5 38.6 24 54 MiddleGuangdong 3,065 8,668 4,663 2,581 18,977 11.9 29.6 25.2 44.41 55 Northeast Guangdong 3,900 2,81 I 8,979 2,030 17,720 15.2 9.6 48.5 3I.21 56 Hainan 1,840 8,590 2,612 1,671 14,713 7.2 29.3 14.1 25.] 57 Kangding-Zoige 11,651 22,205 23,362 2,443 59,661 45 76 126 37.~ 58 Zhongdian >7,900 17,247 17,922 5,256 48,325 30.7 59 97 81 59 Lanpmg Simao >7,900 12,588 11,201 7,953 39,642 30.7 43 60.5 122.3 fSO Baoshan Lancang > 10,230 19,190 7,463 2,551 39,434 39.8 65.5 40.3 39.21 fSl Nmgxla 1,571 12,729 4,778 3,653 22,731 1.2 43.4 26 56.21 fS2 Alxa Longshoushan 9,662 2,356 8,656 493 21,167 7.7 8 46.8 7.6 ~3 Dunhuang-Alxa 14,525 19,801 9,743 663 44,732 11.6 67.6 52.7 10.21 ~4 Qilianshan, Gansu 18,543 27,430 7,988 2,298 56,259 14.8 93.6 43.2 35.41 ~5 Qilianshan, Qinghai 3,547 23,347 4,543 5,308 36,745 2.8 80 24.6 82 fS6 Qmdam 8,354 16,327 7,412 6,803 38,896 6.6 56 40 1051 fS7 lanm 5,879 22,451 4,910 13,782 47,022 4.6 76.6 26.5 21~ 68 Kunlunshan 24,781 19,846 9,039 8,046 61,712 19.7 67.7 49 1241 Kl9 East Kunlun 6,073 11,531 13,034 30,638 4.8 39.4 70.5 -I rO BayanHarShan 6,835 10,811 2,687 20,333 23.3 58 4.11 r1 IanggulaShan 7,424 19,248 5,383 32,055 25.3 104 83 R2 Karakorum Shan 3,904 10,263 2,108 16,275 13.3 55.5 32.41 r3 Qlangtang=Qamdo 11,409 16,587 6,230 34,226 38.9 89.7 95.~ r4 Gandise-Nyainqentanglha 5,607 11,024 2,203 19,474 19 59.6 11 ps Himalaya 8,107 17,917 2,912 31,521 27.7 96.8 44.~

~eferences for Appendix 2

~ureau of Geology and MmeralResources of Provmces (1984=1993) RegIOnal Geology of Provmces. Geological Pub-I Iishmg House,Beljmg(m ChmeseWith Englishabstract, as shownm References for Chapter 1).1 1396 Appendlcesl k\ppendix 3 Dataof Folding andPrincipal Stress Axesof Chinese Continental llectonlc Eventsl

VtPPendix 3.1 Data of folding and principalstressaxesof QinglJaikou Periodl 1(1,000-800 Ma)

LocatIon Foldamount Axes LImb Area al (0) a2(O) a3(O) Long. n Lat. (0) Antic. Sync. Orien. (0) Angle (0) 1104.5 32.3 Pingwu 6 6 80 40-60 350L5 80LI 170L8~ 1106.5 32.3 Nanjiang I I 70 50--75 340LI2 70L3 160L78 1107.5 32.3 Zhengba' I I 50 65-75 320L5 50L2 14018~ 1110 5 323 Zhnshan 1 1 HKI 4JRiO 190/10 10014 10780 1103 5 31 3 Maowen* I I 340 50----70 70/10 340L5 160/80 1110.5 31.7 ShennongJla I I 90 30--85 2L22 90110 181168 1112.5 31.7 Yicheng 5 4 90 20--40 OLIO 90L3 180L80 1113.5 31.7 Shuixian" 16 16 300 40-60 30L9 300L5 21OL811 11145 317 Xinxian" 13 12 319 35-55 49/11 319/6 229L79 1115.5 31.7 shancheng 4 6 115 40=70 2519 11719 251Z77 1116.5 31.3 Lu'an, Yuexi 2 1 90 30=55 018 9011 180182 1114.5 31 HuangpI' 7 5 310 30=65 4115 31012 22018~ 1115.5 31 Luotlan' 3 I 300 50=30 30111 30123 2llZ79 1102.5 30.3 Baoxmg' 1 I 0 50=70 8919 114 270180 1103.5 30.3 Qionglai' I 1 65 40--70 155LI5 65L8 335L7~ 1114.5 30.3 Wuhan' I 1 136 40-65 227LI 137Ll1 317L78 1115.5 30.3 Qichun" 7 6 300 32-58 206L4 295L2 30L85 11165 103 Tajhu 1 1 280 50-70 11131 280/3 192760 1117.5 30.3 Anqmg 2 0 76 60=80 34516 7515 16518~ 1118.5 30.3 Jmgde I 0 92 50--80 IZ15 92L2 181Z7~ 1103.5 29.7 Emei I 0 280 70--85 192L7 280L3 IOL83 1112.5 29.7 Huarong I 1 99 40--50 183L3 269LI4 75L761 III3.5 29.7 Pug. 2 2 285 40=85 195123 28519 15167 1114.5 29.7 Tongshan 3 4 80 50-60 I7714 80121 266Z7~ 1115.5 29.7 Ruichang 2 1 280 35-70 IOL4 280LI 190L86 11165 297 Hukou 7 7 86 30----65 356L20 86LI 176L72 118 29.7 Qimen-Tunxi 7 6 85 36-72 350L29 85LI 175L70 1120.5 29.7 Zhuji' I 0 40 50-60 130LIO 41L9 310182 11025 29 Shjrnjan 1 0 90 6(Ri5 18212 9012 1I8!! 1103.5 29 MabIan 9 9 80 60 35015 8015 17118.'l 1112.5 29 Yuanjiang 2 I 95 50--70 18519 9514 518~ 1113.5 29 Pingjiang 8 7 294 40-60 25LIO 295L4 204L79 11145 29 Xjllshllj 4 4 85 60----70 175L5 8U5 355L86 1115.5 29 Yongxiu 5 3 274 25-45 359LI3 275L15 197L76 III6.5 29 Boyang 2 1 90 40=80 1120 9015 181169 1117.5 29 Lepmg 2 3 85 50=70 17519 85111 3551811 1118.5 29 Quxmn 2 2 100 52=65 015 9116 18118~ 1119.5 29 Jmghua I I 92 20--35 119 9014 182L811 1111.5 28.3 Anhua 6 5 91 50--85 182L13 89L6 OL771 1112.5 28.3 Changsha 4 3 110 50-60 20L5 I1OL2 201L86 1113.5 28.3 Liuyang 2 3 90 25-40 182L4 89LI IL8(j 1ll4.5 28.3 Tonggu 8 8 93 40=85 423 9418 273184 IllS 5 283 (laoan 4 2 78 38 70 347/9 78/1 1777811 1116.5 28.3 Dongxiang 11 12 90 45 75 182214 90110 IZ751 1102.5 27.7 Xlchang I I 80 45 rrrzz 8022 350188 1103.5 27.7 Zhaotong" I I 5 70--80 275L6 5L2 95L85 1108.5 27.7 Jiangkou' I 1 31 60--80 12115 3010 300184 1109.5 27.7 Zhijiang I I 80 30--75 170L23 80LIO 350L77 11125 277 Shaoshan 2 2 92 45 70 179/18 90/12 0172 11145 277 Yichun 1 1 81 60-70 351/10 80/2 170780 f'\ppendix 3 Dataof Foldingand PrincipalStressAxesof ChineseContinental Tectonic Events 3971

Contmued Location Foldamount Axes LImb Area ()I ()2(O) ()](') Long. (0) Lat.j") Antic. Sync. Orien. n Anglen ra) 1116.5 27.7 Nancheng 2 2 100 30=70 1OZ20 100ZIO 191Z72 1117.5 27.7 Guangze I 2 98 55 80 6Z8 98Z15 280Z74 1101.5 27 YanbIan I 2 SO 70-S5 170Z9 SOZ4 351Z73 1102.5 27 Miyi 7 5 2S0 50-60 190L5 2S0L2 IOLS5 1109.5 27 Huitong I 1 70 25-45 IS0Lll 9U5 USI 1117.5 27 Shunchang 3 3 S7 40-60 357L1 S7L5 261LS~ 199.5 26.3 Lanping' I I 350 30-40 260L5 350L3 SOZS61 1101.5 26.3 Yongren* 5 4 40 40-50 31OL5 40L2 130LS4 11025 263 HlIili 2 2 80 55 75 171/10 80/5 351780 1103.5 26.3 Dongchuan" 2 2 2 100SS 271LI5 OLIO 90L75 1117.5 26.3 Sanming 3 1 S2 60-70 165L4 SUS 344LS4 1101.5 25.7 Dahao' I 2 60 40-50 330Z5 60Z4 151ZS:1 1102.5 25.7 Wuding' 2 3 45 35-50 135L7 45L6 315ZS~ III6.5 25.7 Dmgchang 0 I 116 30=35 26Z3 116Z3 252Z86 1101.5 25 Chuxiong* I 0 I 36-45 91L9 1L3 271LS2 1102.5 25 Kunming" 7 6 IS 45-65 105L1O 15L5 2S5LSO 1103.5 25 Yiliang' 10 10 20 40-50 290L6 20L2 1I0LS4 IIOS.5 25 Luocheng 6 5 2S0 50-75 IOL13 2S0L7 190L77 1116.5 25 Shanghang I 0 95 40-76 5L1O 95L5 IS5L79 11025 243 Yuxj* 6 6 0 47-78 270L9 OL4 9U811 11025 237 Ijanshllj 4 4 290 4Jb60 20/11 290/3 202780 1112.5 23.7 Humil 1 I 270 30=72 180Z19 90ZIO 0Z71 1103.5 22.7 Jmpmg' 3 4 310 40=50 220Z5 310Z3 40Z85 1100.5 22.3 Jmghong' 4 3 10 30=60 lOOZI5 IOZ12 280Z74 1100.5 21.7 Menghal' 4 5 30 30=50 330ZIO 30Z6 120Z80 ~ Re-deformation folds by latertectonics. 234 229

[Appendix 3.2 DataoiJoldingandprincipal stress axis oj QUianian Periodl 1(513-397 Ma)

Location Foldamount Axes Limb Area (),n Long. (0) Lat.n Antic. Sync. Orien. (0) Angle (0) ()2n ()3(Ol 1109 193 Hainan Island I 2 40 45-60 130L15 40LI0 310D5 1112 21.6 YangjIang, Guanghm I 3 0 35-75 90Z5 ono 270Z85 109.5 22.3 Lmgshan 4 4 85 40=70 175Z15 85Z12 355Z75 1l0.5 22.3 Yuhn 5 3 19 30=70 109Z8 19Z5 289Z82 1112 22.3 Yangchun, Kmpmg 4 5 5 30-70 95Z15 5Z16 275Z75 107.5 23 Daxin 5 4 90 40-60 IS0L1O 90L5 OLSO 109.5 23 Nanning,Guixian 26 27 76 20-70 166LI5 76L5 346D5 114.5 22.7 Baoan,Huiyang 3 0 20-S0 90LIO OL5 270LSq 105.5 23.7 Funmg I, arc type 80 35=45 170ZIO 80Z7 350Z8Q 1108 23.3 Bmse,Lmbm 8 8 90 30=60 180Z7 90Z5 OZ83 1111 23.7 Gmpmg,Wuzhou 6 5 92 35-80 2Z12 92Z8 182Z781 1113 23.7 Humjl,Chonghua 5 6 51 30-S5 141Z15 51Z1O 321Z75 114.5 23.7 Heyuan 2 2 357 30-65 267D 357L20 170LSCj 1111 24.3 Lipu,Hexian 23 21 S7 40-75 177L15 S7L12 357D5 112.5 24.3 Yangshan 2 2 33 45-70 123LI2 33LlI 303DSI 1114 24.3 Ymgde, Llanpmg 3 3 IS 45 80 105ZIO 15Z8 285Z8Q 115.5 24.3 Xmgnmg 4 4 20 60=85 lIOZI3 20ZIO 290Z771 116.5 24.3 Meixian 3 1 0 30=80 90Z18 OZ5 270Z72 1105 247 GlIilin 2 I 256 42 72 163/12 256724 44/61 111.5 25 Jiangyong S 7 40 50-60 130L53 40LIO IOLS~ 112.5 25 Lianxian l l.arc l l.arc 90 50-SO OLIO 90LS IS0LSCj 113.5 25 Shaoguan 6 6 357 43-60 267LS 357L5 S7LS2 II4.5 25 Longnan 11 5 10 50=80 100Z5 IOZ5 280Z85 1116 25 Xunwu,Shanghang 8 8 10 30=80 lOOZI2 IOZ5 280Z781 1398 Appendices

Contmue(l ocation 0 Area CY2(O) Lon. Lat. CYI ra) CY3ra 117.5 25 Longyan 0 30=50 90710 075 27078q 1113 25.7 GUiyang, ChenxIan 36 110 32 85 20711 110710 2()()27~ 1145 257 GanzhoJl 20 355 40----80 SSZ20 35SZl0 26517(J 1116 25.7 Yudu-Changding 4 180 30-60 90LS 180LIO 270L8S 118.5 25.7 Dehua I 182 60-70 91LS 182LS ILSO 1112 26 Yangmingshan I I 90 30-40 OL5 90L2 180L85 114.5 26.3 Jmggangshan 15 14 350 35 85 260Z20 350Z15 80270 1116 26.3 Xmgguo,Nmghua 7 5 4 35 80 271718 427 103271 1118 26.3 Sanmmg, Nanpmg 5 5 197 25=62 10627 197710 3422781 112.5 27 Hengyang 2 3 110 43-69 200713 11079 2907771 114.5 27 Youxian, Yongxin 9 8 5 30-70 95L5 5LIO 275L85 117.5 27 Guangchang, Jianou II 10 3 45-61 93L8 3L5 273L8:;J 1118 27.7 Guangze, Pucheng 6 6 10 30-80 lOOL25 IOLIO 280L65 119.5 28 LtshUl, Tmshun 3 48 30-80 138720 48715 31827<1 105.7 26.7 Nayong, Zhtjm I 87 14=20 17775 8773 35678G 1101 28.2 Muh 3 2 95 30=40 575 9570 1857841 122.2 43 Wafanggou I 3 55 70-75 14475 5572 32S78~ 125.1 43.5 Gongzhuling I 2 290 45-60 200LIO 290L6 110L8(j 126.2 44.4 Jiutai I 0 300 40-60 211L4 300L4 121L85 1264 429 Hulan 2 2 330 45-70 60L5 330L4 12U85 1272 431 50mb Jiaohe 1 1 20 50-70 11075 20/5 2(K1I85 1286 439 North sJlohua II 0 62-75 9114 0/6 271/841 128.4 43.6 Guan(ll I I 0 40=75 8973 027 26978(J 1285 43 I Antu I 2 320 5!b60 51/3 320/2 2311881 128.5 43 Hanchonggou 0 I 320 55-70 51L5 320L6 230L85 128.6 43 NorthShuguang I 0 320 40-70 SOL4 320L4 230L8§ 1129 42.7 WestLongjing 2 I 340 40-60 70L5 340L5 250L85 1129 42.8 Yanjt 0 1 330 60=70 6272 330Z2 2417881 Il19 431 HIIDchnD 0 I 0 4Jb65 90/4 0/6 270185 1100 38 NorthQthan 3 3 310 60=70 4174 31075 221785 102.2 36.2 LaJlshan I I 280 50-70 19215 280/3 12184 98.4 36.5 NorthQaidam 0 I 290 60-70 200L6 290LIO 20L8~ 1100 38.2 SouthQilian 6 6 292 40-50 202L4 292L5 22L86 P6 38.6 Yueyashan, SouthQilian 4 5 270 60-70 180L3 270L2 OL87 91 37.5 Qlmantag 5 5 90 60 18074 90Z2 0788 P8 39.3 NorthQlhan 6 6 300 50=70 3276 300710 21178~ 98 39 MiddleQilian II II 300 60-70 30L8 302L5 209L83 96 38.7 SouthQilian 3 2 292 60-70 203L5 292L6 22L8~ 878 485 Kasna 6 5 178 70-80 88/6 178/10 268/841 90 47 Kokfokay 4 4 305 70=80 3575 30578 21S78~ 182 42.6 Hark,Ttanshan 10 9 70 60=80 34027 250710 1607841 ~6.2 43 Chaganor, TIanshan 7 6 110 40-70 20216 11079 21781 189 41.3 Kuruktag 17 16 98 40-75 SLIO 98LS IS8L8(j P3 41 Xingxingxia 6 5 128 50-70 37L9 128L12 217L81 189 385 AltunShan 10 9 100 60--180 191L7 100LI0 IILS2 188 375 East Kunlun 5 6 95 4Jl--75 7/5 96/6 187/85 ISO 36 Mjddle Kunlun 4 3 91 55-70 18276 9112 2184 175 38 West Kunlun 18 16 125 50-75 34/8 12517 215181 4211 381 f'\ppendix 3 Data of Folding and Principal Stress Axes of Chinese Continental Tectonic Events 39~

Vtppendix 3.3 Datao.f.folding and principal stress axis 0.[Tianshanian Period; 1(297-260 Ma)

ocanon im Area 0 (J"j(') (J"2(') (J"J(O) Lon. ° Lat. ° Antic. S nco An Ie 90 477 Nort 3 2 310 50-60 40/10 310/7 221/80 89 47 Kelan 6 7 306 50=60 3675 306710 216782 90 46.2 Ertix River 4 5 300 50-75 210/7 300/5 32/80 85.7 47 West Junggar 23 21 285 40-75 16/8 285/8 195/82 90 45.8 East Junggar 21 20 302 50-80 32/10 30219 212180 86 435 North TI'lDsh'lD 12 10 290 60-80 200/4 29076 207861 82 43 Tekes, Tlanshan 13 12 86 55-75 356Z3 8676 176787 86.2 43 Bostenhu, Tlanshan 16 17 100 40-70 974 100Zl0 190786 89 41.3 Kuruktag 12 11 88 45-70 35878 88Z7 178782 93 41 Xingxingxia 6 5 80 40-65 350/5 80/8 170/85 88 375 East Kunlun 14 13 87 50 80 176/6 87/9 356/84 80 36 Middle Kunlun 10 II 122 50 70 20215 29217 22185 75 39 West Kunlun 7 6 110 60 80 4074 311l/1O 220786 97 173 hmW Shan 4 5 90 60 80 180/4 27075 078(J 92 36.2 Erdaogou 6 5 300 64=75 30Z3 300710 210787 96 35.6 Burhan Budm 4 3 290 60 75 20074 29076 207861 99 34.5 Anyemaqen 2 2 300 55-80 210/6 300/5 30/8~ 962 41 8 Beishan 15 14 270 40 70 357/12 268/15 178/80 106 34 Tianshui, Huixian 6 6 88 30-70 177/4 88/5 358/85 11048 B3 WlIdll 8 8 280 40 80 190/8 280/10 10780 ~5.5 39.7 Dunhuang 4 4 82 60 70 35678 82Z6 174782 1103.5 39.5 A1xa 4 5 85 50=60 174Z3 8576 355786 108 42 North Badam Jaran 6 7 90 40-70 178 9175 180782 114 44 Sonid Zuo Qi 8 7 80 35-65 350/6 260/8 172/84 117 45 Ujimqin 11 12 65 35-60 336/5 65/7 155/85 121 48 Songling 9 8 60 40-60 150/4 60/10 331/86 126 51 Huma 6 6 50 35-55 141/6 23578 325784 126 43.3 Shuangyang 8 7 55 30-60 14576 23578 325784 1129.7 43.4 Wangqmg 2 3 52 30=60 322Z5 52Z9 I42Z85 D50 2421

!Appendix 3.4 DataoiJoldingandprincipal stress axis oj Indochina Periodl 1(260-200 Ma)

im Area 0 (J"j (0) (J"2(') (J"J(' An Ie 197.8 Tongtlanhe 6 5 290 75-85 20Z3 29075 200787 100 Qinghai Nanshan 0 I 292 40-65 202/5 29213 22/85 101 Zeku, Tongde 4 3 282 40-60 12/3 28214 193/87 100 Maqen 8 8 290 40-60 201/6 290/10 21/83 93 Fast Kunlun 4 6 280 50 70 10/2 280/6 191/88 98 Bayn Har Shan 6 6 295 45 65 20575 29578 25785 1995 Baima 2 2 302 40 50 212/6 lO2I5 321841 101 North Qlhan 10 9 280 39 60 1176 28075 19078~ 199.5 Middle Qilian 7 8 290 50-70 22/7 290/4 203/8~ 99 South Qilian 10 9 282 20-60 22/5 292/10 202/8~ 1937 Olunbluk I 0 285 40 50 195/2 285/6 15/87 1944 Maoniushan 0 I 280 30 50 191/5 280/8 10/85 91 South Q1mantag 0 1 284 20 30 13Z3 282Z7 192786 1916 East Kunlun I 2 lOO 30 64 2IIII 10 lOO/5 lOlSO 94 Tanggu1a Shan 12 13 290 35=60 2074 290710 202784 1101.9 Menyuan 3 2 300 45-75 208/3 300/8 28/85 fiOO Appendices

Contmuedl ocation xes nn 0 0 Area 0 0 CY! (0) CY2 (') CY](' Lon. Lat. Antic. S nco Orien. An Ie 106 34 Tjanshllj Hujxjan 6 6 88 30 71l 177/4 8815 358I8S 1104.8 33.3 Wudu 8 8 208 40 80 190Z8 280ZIO IOZ80 195.5 39.7 Dunhuang Batushan 4 4 82 60 70 356Z8 82Z6 174Z82 1103.8 36.1 Tianzhu-Jingtai 1 1 100 13-25 190L:2 100LS 1OL:88 79 35.8 Karakorum 14 10 280 35-70 19U4 280L7 IU861 875 365 East Kunlun 8 7 86 35 70 35517 86/9 175183 98 29 Zogang 6 6 335 50 70 65Z5 335Z6 235Z8~ 197.8 31 Qamdo 17 18 150 40 65 61Z6 150ZIO 240Z84 91 32.5 TanggulaShan 10 12 100 40=60 IOZ5 100Z8 190Z8~ ~8.2 34 WestTanggula 7 7 125 40-65 35Z3 125Z6 215Z87 88 35.8 HohxiIShan 2 2 89 30-60 358L4 89L7 179L:86 1126.5 50.3 Jadaqi 4 5 90 30-60 IL7 91L:2 180L:82 1126.5 49.3 Longzhen 11 10 41 25-65 13UI5 40L:3 311L74 11285 47 TIeli 3 4 45 30-65 135/10 4515 314/81l 1129.5 46.3 Hesgula 6 6 60 32=60 329Z6 59Z1 148Z84 1132.5 46.3 Baoqmg I I 46 30-50 136Z8 46Z4 317Z82 122 45.5 Tuquan 8 8 80 28-48 170Z15 80Z3 350Z7~ 1128.5 45.3 Bingxian 8 3 300 32-52 30L:1O 300L:5 21OL:811 1119.5 44 Balin Zuoqi 6 11 75 20-55 345L:14 75L:2 165L:84 126 44 Jilin city 10 9 10 45 35-55 135L:9 45L:3 315L:811 131 43.7 Shuangchengzl 9 4 80 30-50 350Z6 80ZI 170Z84 1129.5 43 Yanjl 8 6 45 40-57 134Z5 45Z5 315Z8~ 118 42.7 ChIfeng 2 I 70 38=65 160ZlO 70Z7 340Z80 11205 423 Xjawa 7 6 81 30-66 352/7 81/2 171 781 126 42 Tonghua 3 8 67 30-62 157L9 67L3 338L811 1104.5 41 Vliji 3 4 88 28-58 178L15 88L4 358L7~ 118 41 Chengde 11 3 83 40-60 173L:8 83L:2 353L:82 1110 5 403 RaotoH 3 4 86 42 62 356/7 86/1 176/8~ 118 40 Tangshan 8 11 93 30 50 4Z8 93Z2 183Z82 1110.2 39.6 Dongsheng II 0 85 32=48 355Z3 85Z1 175Z87 1115.6 39.7 Lmshm25 6 5 85 28-40 175Z18 85Z5 355Z72 1109.5 37 Yan'an 5 0 80 13-20 170L:2 80L:I 350L:88 109 34 Qinling 12 5 92 40-60 19U5 9UI 4U85 1117.5 34.3 Xuzhou 37 36 44 42-65 314L:6 44L:0 134L:84 102 33 Hongyuan 10 8 90 30=45 180ZI5 90Z0 0Z751 1103.5 33 Zhangla 5 2 100 35 55 190ZlO 100Z5 IOZ8(J 109 333 Dahashan 9 7 290 35-65 20/10 290L:l 200L:80 118 33 Bengbu 5 3 260 30-52 350L7 260L:l 170L:8~ 1104.5 32.3 Pmgwu 21 24 75 36-65 165ZlO 75Z6 345Z80 1106.5 32.3 Nanjlang 16 0 82 30=60 172Z5 82Z4 351Z86 119 32.3 Nanjing 56 51 72 30=65 162Z5 72Z3 342Z84 1103.5 31.7 Maowen 17 17 90 28-66 OZ4 90Z2 180Z86 1113.5 31.7 Shuixian 27 27 300 31-55 30L:16 300L:1O 21OL74 1118.5 31.7 Maanshan25 17 16 51 29-54 321L:6 51L:0 l41L:84 109 31.5 Chengkou 12 11 288 30-50 18L4 288L5 199L:8~ 101 30.7 Kangdmg 14 12 90 29-55 OZ5 90Z4 180Z8~ 114 31 Huangbl 18 19 29 30=60 20Z16 290Z7 200Z61 118 31 Xuancheng 24 26 47 29=65 317Z8 47Z1 137Z82 11205 31 3 SlIzhOJJ 15 II 53 28-60 323/5 53/1 143/89 1102.5 30.3 Baoxing 8 8 100 20-50 1OL:5 100L:2 190L:8~ 115 30 Tongshan 23 62 61 90 30-60 180L:14 90L7 0L7§ 117 29.7 Qimen 40 46 85 29-55 176L7 85L:6 355L:82 1120.5 29.7 Zhujl 49 37 58 35 60 328Z5 58ZIO 148Z8~ 101 28 Yongmng 29 31 85 34=65 175Z5 85Z5 355Z8~ 11125 275 Hunan 48 54 88 30=-65 176/7 88/4 356/8~ 115 27.3 Jiangxi 46 47 87 28 66 357Z8 87Z7 177Z8~ 1117.5 26.7 Fujian 14 28 95 20-55 185L:5 95L:5 5L:851 f'\ppendix 3 Data of Foldingand PrincipalStress Axes of ChineseContinentalTectonicEvents 401

Contmuedl

Area CY! (0) CY2 (') CY](' (iujzholJ 18712 97/1 7/881 1107 23.3 Guangxi 100 91 85 32-50 175L:1O 85L:8 355L:80 114 23.5 Guangdong 49 65 89 30-48 359Z15 89Z9 179Z7~ 1100.5 24 Jinggu 42 43 I 40-60 91L:15 1L:6 271L7~ 11055 19 Hainan 0 3 90 35-64 180L:10 90L:5 OLSO Jomt observatIOn pomts 83 1,109 1,086

Vtppendix 3.5 Datao.f.folding and principal stressaxisofYanshanian Period; 1(200-135 Ma)

ocation xes 1m 0 Area 0 CY! (0) CY2(O) cy](O) Lon. Lat. ° Orien. ° An Ie 126 50 Longzhen 8 24 25-50 294Z5 24Z3 114Z8~ 1285 47 Tieli 0 30 30-55 120/3 30/6 3oo78J 132.5 46.3 Baoqing 0 25 30-50 115L:6 25L:5 295L:8~ 119.5 46.3 Hesgula 3 14 28-52 284L:5 14L:3 104L:8~ 121 45.7 Tuguan 17 35 25-54 305L:5 35L:4 125L:8~ 1275 45 1 BinxlGuangzhou 41 29 30=65 119Z18 29ZIO 308Z721 85.7 46 Krarnay I 50 20 30 140Z20 50Z5 320Z7q Joint observationpoints 168 1,566 fi02 Appendices

Vtppendix 3.6 Data o.f.folding and principalstressaxis 0.[Sichuanian Periods 1(135-56 Ma)

Locallon rold amount Axes LImb Area (J"I(') (J"z(O) (J"J(O) Long. n Lat. (0) Antic. Sync. Orien. (0) Angle (') 908 386 Xorkllii 8 8 90 60--85 2/2 90/85 2711J 99.1 38.1 Muh 2 2 280 25-52 19076 280710 10782 fJI 34 upper Tuotuo River 2 2 285 30--60 195/3 285/5 10/851 fJ2 33.3 Wenquan 6 6 290 40--60 200/8 290/4 20/851 94.2 33.3 Moyun 7 7 294 30--50 24/6 294/4 204/841 1032 363 Mjnhe-HekQII 10 7 288 21l-1O 19Z7 288710 19978] 104.2 35.1 Wciyuan 1 1 290 20=30 20Z3 29075 2007871 D1 32.5 Tanggula 7 8 100 40=65 1075 10078 190785 85 33 Dinggu 3 3 93 40--60 183Z2 9376 3788 81 34 Zapug 19 18 90 40--60 1/6 90/5 181/841 fJ3 31 Nyainqentanglha 17 18 93 30--70 3/4 93/7 183/8§ 85 31 Cogen 15 15 92 30-70 2/6 92/5 182/841 124.5 51 Songhng 1 6 83 10=35 353711 8374 173Z781 121l5 457 Tulemaotu 3 355/1 8572 175185 1125 46 SonghuaJlang LIaohe 11 0 296 0.5 5 2672 29671 20678~ 119.5 44 Ba1mZuoql 4 5 102 I 32 1223 10222 1922871 1130 43.5 Yanbian 0 9 112 5-33 22/9 112/2 202/81 1115 43 Liaoyuan 7 0 315 4-32 225/6 315/6 45/8~ 1185 43 Wllfendi 3 5 290 2 32 20/15 290/6 200/75 1125 43 Slpmg 12 4 0 318 4=32 48Z3 31872 2287871 121 8 42 FlIxjn 16 2 2 162 1Il-32 252110 16211 n/81l 118.5 41.7 HargmQI 2 1 115 10=32 25Z3 11571 2057871 104.5 40.5 UhJI 4 6 111 12-32 221Z2 111/1 2178~ 115.5 40.7 Longguan 17 6 7 308 12-32 38/1 308/1 216/881 109.5 39.7 Dongsheng 40 19 98 15-30 8/2 98/4 186/8§ 1119 40 Qinhuangdao 6 7 295 20--40 25/15 295/7 206/8Q 108.5 38.7 Urad Qlangl 20 4 310 20=40 4076 31072 2207871 1112 38 Shanxi 3 3 284 21l-1O 196/1 284/2 102/871 120.2 37 Zhaoyuan-YexIan 14 I 1 122 15-30 30718 122710 240Z7<1 1103 36.4 Lanzhou 5 7 112 20--36 2371 11221 2967881 107.5 35.1 Huanxian 18 1 308 20--30 218/4 308/4 38/851 118.5 36 Middle Shandong 82 12 12 299 10--32 29/6 299/3 206/821 1113 34 Henan 10 4 3 106 15-30 196/12 106/3 16/771 117.5 33.5 Bengbu 6 8 321 10=35 51Z3 32171 2317871 1102 32 Markam 48 42 310 25=40 411/6 31011 2211/85 1106 32 Yllong 85 43 292 20=40 20275 29271 227851 1109 32 Dabashan 13 84 76 285 20--40 15714 28573 195Z7(j 1111 31.5 Hubei 31 120 105 288 22-45 18/2 288/3 108/871 117.5 31.3 Jiangsu-Anhui 25 77 65 115 20--35 205/2 115/2 205/881 103 5 293 West Sichuan 83 52 107 22 36 17/3 107/1 197/871 1120 29 ZhejIang 29 21 36 295 20=34 25Z3 29575 2057871 1023 267 Yanbjan 69 81l 302 25dJ) 210/6 302/2 1078~ 105.3 25.3 LmpanshUl 15 13 310 25=44 22075 31072 4078~ 1112 27.5 Hunan 18 7 12 123 20--50 213Z2 12379 315780 115.7 26.3 Jiangxi 12 33 120 20--50 220/3 120/12 40/81 117.5 26.3 Fujian 11 6 27 122 20--54 31/6 122/5 262/821 1102 23.7 Yuxi 122 137 301 30--60 211/10 301/4 31/80 1114 23.7 Guangdong 10 22 295 20--50 205711 29573 26Z7~ 109.2 22.5 Guixian 12 31 121 24-50 31/4 121/3 212/8(j 1093 195 Hajnan 1 1 335 25-50 241/1 335/25 150/65 281 1,032 97~ EJomt observatIOn pomts f'\ppendix 3 Data of Foldingand PrincipalStress Axes of ChineseContinentalTectonicEvents 403

[Appendix 3.7 Dataofjolding andprincipal stress axis oj NorthSinian Periodl 1(56-23 Ma)

Location Foldamount Axes Limb Area 0"1 (0) 0"2(°) Long. (') Lat. to) Antic. Sync. Orien. (0) Angle (') 0"](°1 128 48 Heilongjiang 2 8 28 0.5-10 118L8 28L5 298L8 II 124 46 Songhua)lang-Nen]1ang 116 110 10 0.5=6 100Zl 1072 280788 127 43 Jilin 12 21 205 2 32 295/8 20574 251821 122 41 LowerLiao River 19 12 10 27 2 33 29773 27Z2 117787 108 40 HangginQi 8 5 4 0.5-18 9473 18471 274787 106 37 Ningxia 22 20 5 0.5-20 96",2 5",2 275",88 1103.9 35.9 South Lanzhou I 0 178 20-30 86",4 175L7 265"'8.:l 1104.2 36.3 East Liuhuangshan 0 I 15 20-30 106",6 15",10 285",82 1969 39 Ej-lsl Vemj-lShj-lD I 0 183 20-30 274/4 18376 94/8~ 1972 396 Vurnenhanxja I 0 180 30:;40 0/5 180/4 92180 1118.5 36.5 Shandong24 6 5 26 10=50 115712 26Z3 298Z78 1121.5 34 SouthHuanghai 39 30 9 0.5-28 9971 18973 279788 120 33 NorthJiangsu 49 45 175 0.5-30 85",2 175",2 265",87 105 32.5 Guangyuan 33 28 25 2-30 115",10 25",4 295",80 103 31 Guanxian 82 77 40 2-33 130",9 40L3 31OLSO 11125 312 Huhei 12 4 3 9 5-35 279/5 9/3 99185 119 32 Nanjmg25 2 5 20 4-33 11075 2074 29078~ 1101.5 30 Kangdmg 78 82 8 6-32 98712 18875 278Z78 1107.5 30 Daxian 86 72 28 6-32 298714 2876 118Z7j 102 29 Mianning 107 110 1 2-34 91",10 181",4 271",80 120 29 Zhejiang35 4 3 17 2-31 287L4 197L5 107L86 102 263 Huili 110 132 2 2 36 27U9 18US 9U80 III 27 HJJmlD 6 15 19 10-32 109/7 199/4 289/82 116 27 Jlangxl-Fujlan 6 6 184 6 32 9476 18474 27478~ 199.5 24 Fengqmg 133 142 7 10=40 277710 7Z2 9778q 11025 243 Yuxj 48 45 356 14---44 86/7 356/3 266781 1100.5 22 Jinghong 55 55 8 12-46 278LII 188L4 98L78 113 23 Guangdong-Guangxi 10 17 5 10-36 95",6 5",1 275",84 114 20.5 Mouthof Zhujiang 10 36 170 2-32 80",1 170",1 260",89 Jomt observatIOn pomts 115 1,043 1,083 lAfJpendix 3.8 Datao.f.folding and principal stress axis ofHimalayan Period 1(23-0.78Ma]

Area 0"1 (0) 0"2(°) 0"](0) 98.4 Ulan I 300 0.5 22 3075 30075 2107851 100.5 Middle Qilian 0 280 10-32 190",4 280",6 10",86 975 VUIDeD 4 300 10-40 3U6 30U4 21OLS4I 104.2 Dingxi I 305 10-32 35",5 305",3 215",851 n06 Hujxjan 0 70 20dO 34074 70Z5 160/8B 102.7 Jmchang 0 280 0.5-20 1076 28076 19078~ 179 Kepmg 6 60=110 10-70 175Z3 8575 3557871 175 Wuqta 5 70-112 10-75 18175 9178 1785 ~2 Kuqa 3 80 10-70 170",6 80",4 350",851 178 Yecheng 2 115 12-68 195",4 115",6 15",86 §2.2 Minfeng I 86 10-65 176",4 86",4 356",851 89 East Kunlun 2 HKI 16-60 180/5 HKl/5 0/85 93 Xmgxmgxla 5 80=100 IS-50 17873 8876 3587871 9 1 East HImalaya 6 95 40-50 18676 95Z7 57841 ~6 Middle Himalaya 8 102 40=60 19214 10215 12186 fi04 Appendices

Contmuedl ocanon 0 Area ()\ (') ()2 (") ()3(') Lon. Lat. BO 31 WestHimalaya 240Z5 150Z6 60Z8~ ~1 32 Gegym 208Z7 118Z6 28Z82 ~5 31 Coqen 2Z7 92Z5 182Z8~ P3 31 Nyainqentangulha 3.i4 93L7 183.i8(j ~I 34 Zapug 1.i6 90.i5 181.i841 ~5 33 Dinggu 183.i2 93.i6 3.i88 pI 32.5 Tanggula IOZ5 lOOZ8 190Z851 122.3 41.2 Llaonmg 166Z30 257Z3 352Z6Q 1106 37 Ningxia 202Z3 292Z2 22Z81 116.5 38.7 Huanghua 1OZ2 100ZI 280Z8~ 118.5 35.8 MiddleShandong 40 174.i1O 85.i1O 297L751 [I8 37.2 Guangji 8 6 77 0.5-15 167L3 77.i1 346.i8~ lOS 5 29 Sichuan-Guizhou II 10 90 05-20 180.i6 90.i4 0.i85 1115 11 Huhei 1 2 277 05-16 18878 277/1 91/82 1]7 5 31 Anhnj 0 1 91 05-19 0/5 9112 182/851 122.5 32.5 SouthHuanghm 41 30 85 0.5-20 175Z2 85Z1 356Z8~ 119.5 33.5 NorthJiangsu 19 17 90 0.5-20 0Z3 90Z3 180Z871 119.5 29 Zhejiang 2 1 273 0.5-14 3.i4 273.i1 98L86 [12 28.5 Hunan 7 8 94 0.5-20 4.i2 94.i12 273L7ll 115.5 27.5 Jiangxi 6 6 269 0.5-16 359.i4 269.i5 178L831 P8 25.5 Fujlan9 181Z7 272Zl2 356Z7~ n02 25 Yunnan 9 14 16 110 05-26 20178 1lOll 29118:1 1108 23 GuangxI 0 7 262 0.5-20 352Z4 262Z2 82Z89 1113 23 Guangdong I 4 85 0.5-20 175Z5 85Z2 355Z871 [loint observation points58 247 222

IReferences for Appendix 3

Bureau of Geologyand MineralResources of Provinces (1984-1993) Regional Geologyof Provinces. Geological Pub-I lishingHouse,Beijing(in ChinesewithEnglishabstract,as shownin References for Chapter 1).1 ~ppendlX 4 DIfferentIal StressMagmtude of ChInese ContInent InMesozoic CenozOIc 405 k\ppendix 4 Differential Stress Magnitnde of Chinese Continent in Mesozoic-Cenozoicl

VtPPendix 4.1 Indochina Tectonic Period

laverage value of differential stress (1\.0") (111) 105.5MPal Iectomc Area Long.°E Lat. oN Rock Oeternuned Sample1\.0" (MPa) Sources Period Mineral IndochIna Lower& Middle 116 30 gramtOld quartz 20 113.2 Wan IF et al.,1997 Yangtze IndochIna Jlaonan, Shandong 119.5 35.5 my10mte quartz 5 104.5 ZhangCH etal., 1993 Indochina NorthHuaiyang 114.5 32 mylonite quartz 16 147 XiongCY et aI., 19921 IndochIna XIncheng-Huangpl 114.5 31 mylomte quartz 6 125.3 XIOng CY et aI., 19921 Indochina Fengxian, Shaanxi 106.5 34 mylonite quartz 4 142 Wang GH, 1993 IndochIna Jmhng,lIangxl 115 28.5 faultrock quartz 41 83.6 LIOW,19851 Indochina Hetai,Guangdong 112.5 23.5 mylonite quartz 2 59 ZhangBY et al.,19941 Indochina Ailaoshan, Cangyuan 101.5 24 granitoid quartz 2 94 WanTF et aI., 199] IndochIna EastGansu 105.5 33.5 gramtOld quartz 9 69.3 WanTF et al.,1991 IndochIna Altun 92 37 gramtOld quartz 1 125.8 Wan IF et a1.,199] IndochIna Eest Kunlun 94 35.7 gramtOld quartz 2 84.6 Wan IF et a1.,199] IndochIna Burang 81.3 30.2 ultramafic rock ohvIne 3 118 ZhaoCH 1 (unpubhshed)

VtPPendix 4.2 Yanshanian Tectonic Period

average value of differential stress (1\.0") (70) 99.4MPa ectomc Area Long.'ELat. 'N Rock SampleAc (MPa) Sources Period Yanshanian Nandazhai, Beijing 116 39.8 mylonite 4 101.8 WanTF et aI., 1997 YanshamanOahelshan, JIlIn 125 43.6 granllmd 3 112.5 LInJP et aI., 1994 Yanshaman Zhaoyuan-YexIan, 120.3 37.2 gramtOld 3 82.5 WanIF, 1992 shandongl Yanshaman MengyIn, Shandong 118 35.7 method of angle 15 82.6 YInXH,1987 Iconjugatel Yanshanian Lower& Middle 116 30 granitoid quartz 14 93.6 WanTF, 1993 Yangtze' Yanshanian Fujian 118 26 granitoid quartz 12 94.6 Lin JP et aI., 1990 Yanshaman Nandan, GuangxI 107.5 25 gramtOld quartz 5 87.7 WanTF et aI., 1997 Yanshaman EastGansu 105.5 33.5 gramtOld quartz 4 71.6 Wan IF et aI., 1997 YanshamanEast QInghaI 101 36 granllmd quartz 3 73.8 Wan IF et aI., 1997 Yanshanian Altun 92 37 granitoid quartz 2 79.5 WanTF et aI., 1997 Yanshaman West Kunlun 75.5 37 gramtOld quartz 1 81.5 WanIF et aI., 1997 Yanshaman EastXizang 96 31 schISt quartz 2 135.6 Wang GH(unpubhshedj Yanshaman SouthXizang 89 29 meta.sandstone quartz 2 130.4 Guo I Yet aI., 198~ f4ppendix 4.3 Sichuanian Tectonic Period;

average valueof differential stress (1\.0") (176) 107.4MPa

ectomc Area Long.'ELat. 'N Rock Sample1\.0" (MPa) Sources Period Sichuanian Daheishan, Jilin 125 43.6 granitoid 19 102.1 Lin JP et aI., 19941 Sichuanian Nandazhai, Beijing 116 39.8 methodof 17 98.3 WanTF, 1981 FUXIn, LiaonIng 122 42 conjugate angle 16 94.2 WuCL et al.,19841 Xikuangshan Hunan 111.5 27.8 28 120.2 Wan CL, 1993 fW6 Appendlcesl

Continued

Tectomc Area Long.'ELat. 'N Rock Determme SampleAo (MPa) Sources Period Mineral Slchuaman NorthHebel 116 41.7 gramtOld quartz 2 88.1 WanTF et aI., 19971 Sichuanian EastShandong 121 37 granitoid quartz 7 81.8 WanTF, 19921 Slchuaman Ian-Lu fault 118.7 36 fault rock Quartz 4 113.5 Wan IF et aI., 19971 Sichuanian WestShandong 117.7 36.2 granitoid quartz 14 77.8 WanTF, 19921 Sichuanian Lower& Middle 116 30 granitoid quartz 16 90.3 WanTF,1993 Yangtze Sichuanian Linhai,Zhejiang 121 28.8 granitoid quartz 17 81.7 ChuMJ et aI., 1988 Slchuaman FUJlan 118 26 gramtOld quartz 9 86.3 Wan IF, 1993 Slchuaman Iongbarshan 113.7 32.3 mylomte quartz 3 140.5 XIOng CY et aI., 1992 Slchuaman XlOngershan 111.7 34.4 vren quartz 2 121.1 Wan IF et aI., 19971 Sichuanian Mangling, Qinling 108.7 33.7 granitoid quartz 2 147 Chai YC, 198(1 Sichuanian Deyang, Sichuan 104.4 31.2 sanstone secendary 9 60.8 ZhangSR et aI.,2003 f1uartz Slchuaman West Yunnan 98.5 25 gramtOld quartz 4 121.5 Wan IF et aI., 19971 Sichuanian Altun 92.5 39 granitoid quartz I 102.5 WanTF et aI., 19971 Sichuanian WestKunlun 75.5 37 granitoid quartz 4 92.5 WanTF et aI., 19971 Slchuaman All & Yarlung zangbo 83 31 sandstone secondary 5 183.5 WanTF et aI., 19971 guartz Slchuaman Southeast XIzang 91 29 pendotlte olIVIne 6 103.7 ZhaoCH(unpublished) xenolIth

[Appendix 4.5 Himalayan Tectonic Period

average value of differential stress (!l0")in upper crust (18) 92.6 MP~

ectoruc Area Long.'E Lat. 'N Rock Determine Sample!l0"(MPa) Sources HImalayan Kuocangshan 121 28.8 1ntermedlate- quartz 2 89.4 Chu MJ et aI., 198~ acid Imagmatltel HImalayan 'Iengchong 98.5 25 gramtOld quartz 2 84.7 Yan OF, 19911 HImalayan Malanshan QInghaI 91 35.8 rhyolIte quartz 105.3 Wan IFetal., 19971 Himalayan WestKunlun 75.5 37 granitoid quartz 2 82.7 WanTF et aI., 19971 Himalayan SouthXizang 89 29 granitoid quartz 7 83.8 ZhaoCH(unpublished) Himalayan Ali 80 32 granitoid quartz 4 109.8 GuoTY et al.,198~ f'\ppendix 4 Differential Stress Magnitudeof ChineseContinentin Mesozoic-Cenozoic 4071 Vtppendix 4.6 Following data arethe d{{erentail stresses determined from the ~nclusion ofmantlein Himalayan PeriotA

average value of differential stress (~O") in mantel (24) 21.5 MPal Iectomc Area Long. °E Lat. oN Rock Determined Sample ~O" (MPa) Sources Period Mineral Himalayan Darnaping, Hebei 114.5 41 iherzolite olivine 5 21.4 Pan SA, 1989 Himalayan Shanwang,Shandong 119 36.5 lherzolIte olIvine 2 29.5 Pan SA, 1989 Himalayan Nvshan,Anhm 118.8 32.2 lherzolIte olIvine 5 17.8 Pan SA, 1989 Himalayan Dangtu,Anhm 118.5 31.6 lherzolIte ohvme I 11.5 Sun P et a!., 1994 Himalayan Liuhe,Jiangsu 119 32.2 iherzolite olivine I 10.9 Sun Pet al., 1994 Himalayan Mingxi,Fujian 117.2 26.3 iherzolite olivine 5 29.7 Peng SB et al., 199q Himalayan Changle,Fujian 119.5 26 iherzolite olivine 3 16 Peng SB et al., 199q Himalayan Lelzhoupenensula 110 21 lherzolIte ohvme 4 14.5 Peng SB et a!., 199(J f4ppendix 4.7 Following data arethe recentdiferential stresses determined by hydrofracturing test

[5 areas average differential stress (~O") 20.9 MPal Determined ITectonic Area No. ~O" (MPa) Sources Period Depth Neotectomc Daglng Oil held 2,000 m± 7 12.5 Chen ZD et a!., 2002 Neotectonic Fuyu Jilin 2,000 m± 14.8 CNC, IUGG, 1983 Neotectonic YingkouLiaoning 2,000m± 22 CNC, IUGG, 1983 Neotectonic DagangTianjin 2,000 m± 18.2 CNC, IUGG, 1983 Neotectonic ShengliOil Field 2,000 m± 12.6 CNC,ruoo, 1983 Neotectonic Dashmkeng, NmgxIa 2,000 m± 19.7 CNC, IOGG, 1983 Neotectonic Qmgyang,Nmgxla 2,000 m± 25 CNC, IOGG, 1983 Neotectonic JIangdu,Jlangsu 2,000m± 24.1 CNC, LUGG, 1983 Neotectonic Qingjiang,Hubei 2,000 m± 22.8 CNC, IUGG, 1983 Neotectonic Zigong, Sichuan 2,000m± 32.6 CNC, IUGG, 1983 Neotectonic Deyang,Sichuan 2,000 m± 12 11.9 WuZJ, 200~ Neotectonic Baise, Guangxi 2,000 m± 25.8 CNC,ruoo, 1983 Neotectonic Sanshm,Guangdong 2,000 m± 40 CNC, IOGG, 1983 Neotectomc Yumen, Gansu 2,000 m± 22.4 CNC, IOGG, 1983 Neotectonic Karamay 2,000m± 8.8 CNC, LUGG, 1983

IReferences for Appendix 4

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IYm YH (1987) Ihe MesozOIC and CenozOIc tectomcstress field01Mengym basmm Shandong Provmce.CollectIon ofj Structural Geology(7): 107-121.Geological Publishing House,Beijing(in ChinesewithEnglishabstract). Zhang BY,YuHN (1994)Deep-seated nappestructureof Hercynian-Indochina CollisionZonein WestGuangdong. Geo-I logicalPublishing House,Beijing] ZhangCH,Gu DL,SongHL (1993)A studyof theleft-lateral normalslip ductileshearzonein thenorthmarginof Jiaonart uplift.Geoscience 7(4): 435-443 (in ChinesewithEnglishabstract).1 ghang ML (1998)StudIeson the IectomcEvolutIOn and the Stressheld of the Qmdarn Basmm Meso-CenozOIc Era. 1M PhD thesIS of Chma UmversIty of GeOSCIences, Beljmg(m ChmeseWIth EnglIshabstract).1 ghang SR, WanTF (2003)Researchon Tectonic StressField and Prediction of FissureZone at UpperTriassicsystem,irj Xiaoquan-Xinchang, Sichuan. ChinaUniversity of Geosciences (an unpublished report in Chinese). ~ppendlX 5 IntraplateDeformatIOn VelocIty of Tectonic Penods InChIneseContInent SInceMesoproterozoic 40~ k\ppendix 5 Intraplate Deformation Velocity of Tectonic Periods in Chinese ~ontinent SinceMesoproterozoiq

[he rock chemistrydata are collectedfrom regional geologyof provinces and regionalgeological survey(I :200,(00), fori calculation of the deformation (extension or shortening) velocity]

IAPpendix 5.1 Intraplate deformation velocity ofMesoproterozoic (1.8-1.0 Ga]

DeformatIOn velocletyl IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing)(cm/yr) Tangshan, Hebel BaSIC volcamc 2 Early MesoproterozOlc 0.12 Jixian,Hebei Basic volcanic 3 Early Mesoproterozoic -0.17 Damiao,Hebei Anorthosite 37 Early Mesoproterozoic -0.23 Liaoning Gabbro 5 Early Mesoproterozoic -0.45 BayanObo rift, InnerMongolia Basic volcanic 13 > 1,600 -O.~ WestQinling,Gansu Basic volcanic 6 Early Mesoproterozoic -0.73 Qlhan, Gansu BasIcvolcaOlc 6 Early Mesoproterozolc -0.46 XlOngershan-Kuanpmg, ShanxI Basalt 22 Early MesoproterozOlc -0.64 Fangcheng, Henan Basic volcanic 2 1,489 -0.] Dabieshan, Hubei Ultramafic 3 Early Mesoproterozoic -O.~ Yunyang-Wudangshan, Hubei Ultramafic 5 Early Mesoproterozoic -O.~ !Shennongjla Dahongshan, Hubel Ultramafic 2 Early MesoproterozOlc Baotan,GuangxI Ultramafic 16 Early MesoproterozOlc 0.] Guangxi Basic volcanic 4 Early Mesoproterozoic Zhuji,Zhejiang Homblendite 8 Early Mesoproterozoic Altun BasIcvolcamc Early MesoproterozOlc O.~ Hark, Itanshan BasIcvolcaOlc Early MesoproterozOlc 0.21 Kuruktag, XInjIang BasIcvolcanIC 2 Early MesoproterozOlc 0.41 Kangbao, Hebel GranItOId 1,468 2.~ Mlyun,BeIjIng GramtOld 10 1,588 61 Liaoning GraOltOld IO 1,565 1,305 6.31 Shimengou, Liaoning Granitoid I Early Mesoproterozoic 6.~ Sandaoqiao, InnerMongolia Granitoid 5 Early Mesoproterozoic 8.71 Dengkou, InnerMongolia Rhyolite 5 Early Mesoproterozoic 8.~ Wuhal, InnerMongoha GraOltOld 16 1,500=1,714 6.51 BayanBleh, InnerMongoha GranItOId 4 1,681-1,696 5.81 ZartayRtft, InnerMongoha AndesIte-rhyohte 8 > 1,600 2.71 BayanObonit, InnerMongoha GraOltOld 8 > 1,600 2.71 AlxaZuoqi Granitoid 6 1,689 7.81 Songji-Lushi, Henan Granitoid 14 1,508-1,631 4.51 ZhonglIaoshan, Henan AndesiteIn land 23 Early MesoproterozOlc 3.31 XlOngershan, Henan AndesIte In sea 48 Early MesoproterozOlc 4.81 !South ShaanxI GranItOId 12 Early MesoproterozOlc 5.~ HuanglIng, Hubel GramtOld 8 Early MesoproterozOlc 5.~ Jiuling,Jiangxi Granitoid 7 Early Mesoproterozoic 7.81 Gate of Qaidam,Altun Diorite 3 1,474 3 Kongurshan, WestKunlun Andesite-rhyolite 6 Early Mesoproterozoic 7·41 Qinling,Shaanxi Basalt 34 1,400-1,000 -O.§ InnerMongoha GabbrOld 4 Late MesoproterozOlc O.~ Altun BaSIC volcamc 7 Late MesoproterozOlc 0.41 Kongurshan, WestKunlun BaSIC voIcamc Late MesoproterozOlc 0.] NorthHunan GabbrOld 16 Late Mesoproterozoic InnerMongolia Diorite 3 Late Mesoproterozoic Hatzhou, Jlangsu Andeslte-rhyohte 4 Late MesoproterozOlc 4·41 Appendices

DeformatIOn veloc.etyl IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) Dabieshan, Hubei Granitoid 8 Late Mesoproterozoic 5.~ Hannan-Tiechuanshan, Shaanxi Granitoid 32 1,400-1,000 6.81 South ShaanXl DacIte 2 1,400=1 ,000 7.~ Dunhuang, Gansu GramtOld 2 1,079 5.11 Kongurshan, WestKunlun Andesile-rhyohte 4 Late MesoproterozOlc 7.§ NorthSIchuan Alkahte 13 1,400-1,000 2.81 Fanjmgshan, Gmzhou GramtOld 54 1,400=1,000 7.31 Fanjingshan, Guizhou Andesite-rhyolite 17 1,400-1,000 4.71 Motianling, Northern Guangxi Granitoid 44 1,400-1,000 7.81 GuangXI Andeslte-rhyohte 2 Late MesoproterozOlc 8 GuangXI GramtOld 3 Late MesoproterozOlc 7.81 NorthHunan GramtOld 3 Late MesoproterozOlc 7.~ YIfeng]langxI Andesile-rhyohte Late MesoproterozOlc 6.§

[Appendix 5.2 Intraplate deformation velocity ofNeoproterozoic-Early Cambrian 1(1.0 Ga-513MaJ

DeformatIOn veloc.etyl IS extension, ea Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) YJ1an-Zhangguangcmhng, Serpentlmte 11 Early Qmgbmkou 0.94 HellongjJan~ Alatan,InnerMongoha Andesile 4 1,056=899 -O.~ Liiliangshan, Shanxi Basalt-andesite 2 Early Qingbaikou -0.49 Xixiang,Shaanxi Basalt 16 1,000-800 -0.56 Fanjingshan, Guizhou Basalt 25 ~ 1,000 -1.1 Sanmen,Guangxi Basalt 3 1,000-800 -0.59 SanmenGuangxI Ultramafic 19 1,000=800 -0.93 Dableshan, Hubel Basalt 80 1,000-800 -0.51 BouderamongAnhm,Zhe]1ang Basalt 5 916 -0.55 and Jiangxj Fengcheng, Jiangxi Basic volcanic 56 Early Qingbaikou -O.~ Gate of Qaidam,Altun Granitoid 26 Early Qingbaikou 41 Daluom.zhen, Hetlongjlang GramtOld 8 Early Qmgbmkou 7.11 Mudanjlang, HeJ10ngjlang Granilmd 5 930 5.11 Shuanghe, HeIlongjIang Granilmd 10 Early Qmgbmkou 4.§ Zhongt13oshan, ShanXI Andesile 40 Early Qmgbmkou 5.81 Shuanyazitun, Heilongjiang Granitoid 6 LateQingbaikou 6.81 Shenxianling, Shanxi Granitoid 6 Late Qingbaikou 6.41 Dableshan, Hubel GramtOld 17 1,000=800 7.81 Xixiang,Shaanxi Rhyolite II 1,000-800 6.31 Erlangpmg, ShaanxI ACId volcamc 33 Late Qmgbmkou 6.~ Maodang, ShaanxI ACId volcamc 39 1,000=800 5.§ Dunhuang, Gansu Granitoid I 790 4.81 Altun,Xinjiang Granitoid 41 1,000-800 6.31 WestKunlun, Xmjlang Granilmd 19 1,000=800 6.51 Kuruktag, Xmjlang Granilmd 17 1,000=800 5.51 l'1anshan, Xmj13ng GramtOld 4 1,000=800 6.~ Pengcheng-Guanxian, Sichuan Granitoid 14 1,043-808 5.~ Huangling, Hubei Granitoid 6 847-879 6.71 SoutheastGmzhou GramtOld 44 Qmgbalkou 7.~ ~ppendlX 5 IntraplateDeformatIOn VelocIty of TectonicPenods In ChIneseContInentSInceMesoproterozoic 4II

ContInuedl DeformatIon velocletyl IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) Fanjingshan, Guizhou Alaskite 54 966 7.~ Yuanbaoshan, Guangxi Granitoid 5 Qingbaikou 7.(1 Sanmen,Guangxi Acid volcanic 8 Qingbaikou 5.~ JIUIIng, Jlangxl GramtOld 19 838-844 6.~ Bouder among AnhuI,Zhejlang Rhyohte 15 818 3.~ and Jlangxll Xiuning,Anhui Granitoid 17 913 7.11 NorthwestZhejiang Granitoid 8 1,00D-800 6.51 Mayuan,Fujian Rhyolite 24 Qingbaikou 6.~ Huma-Jixi,Heilongjiang Ultramafic 54 Nanhua -0.45 ZhangguangcaIhng, Hellongl'ang Ultramafic 46 Nanhua -0.88 Subel, Gansu Basalt I Nanhua -0.34 Yaohnghe, WestHubel-South Basalt I3 800-700 -0.55 IShaanxiI Hunan Basalt 4 Nanhua -0.9 WestGuangdong-Hainan Basalt 2 Nanhua -0.(1 Fujian Basalt 22 Nanhua -0.52 PIngxIang Guangfeng,JIangxI Basalt I Nanhua 0.75 Ymyangguan, GuangxI BasIcvolcamc 4 Nanhua 0.22 Qmhng, Henan GramtOld 24 747 606 5.81 ZhejIang GramtOld 8 844 766 6.~ Rongshui-Sanfang, Guangxi Granitoid 39 730-712 6.11 Xiuning,Anhui Granitoid 4 Sinian 6·41 Hutieling,Heilongjiang Granitoid 68 Sinian 6·41 Vanchangbelshan, Altun DlOnte 3 674.6 7 Vaohnghe, WestHubel South Rhyohte 24 800 540 5.31 IShaanxiI Henan Granitoid 7 593-541 5.71 Fujlan Rhyohte 47 Slman 4·41 JrangxI DecIte-rhyohte 4 SInIan 4.71 Ymgyangguan, GuangxI DecIte-rhyohte 10 SInIan 4.71 Guangdong Declte-rhyohte I SInIan 5.03 lLlQ(J

[Appendix 5.3 Intraplate deformation velocity of QUianian Period (513-397 MaJI

DeformatIOn velocletyl IS extension, ea Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) XInglonggou=QIngshankou, Gabbro 22 Cambnan 0.72 HeIlongjIang] Kedanshan-Xiaosongshan, Ultramafic II Cambrian -1.1 Inner Mongoliel Tongziba, North Qilian Ultramafic I Cambrian -0.73 BaIJIngsl, North Qlhan Ultramafic 12 Cambnan 0.78 Vushlgou, North Qlhan Ultramafic 10 Cambnan 0.86 La!lshan,Qmghar Ultramafic 12 Cambnan 0.75 Barymchang, NorthQlhan Maficvolcamc 10 M. Cambnan -0.57 Zhongwel,Ningxia Maficvolcamc 5 M. Cambnan -O.~ Danfeng,NorthQinling Basalt 5 543-500 -0.28 Heihe, North Qinling Basalt 6 543-500 -0.23 Erlangping,North Qinling Basalt 4 543-500 -0.23 fil2 Appendices

Contmuedl DeformatIOn velocletyl IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing)(cm/yr) Yunjiashan, NorthQinling Basalt 3 543-500 -0.21 Fengxian, Shaanxi Basalt 15 Ordovician -O.~ NorthQinling,Gansu Maficvolcanic 3 E.Ordovician -0.26 NorthQmlmg,Gansu Maficvolcamc 8 M. OrdOVICIan 0.49 NorthQmlmg,Gansu Maficvolcamc I E. Sllunan 0.77 Baijiazui, Qmlmg,Gansu Ultramafic 4 OrdOVICian 0.83 NE borderof Qiadam Ultramafic 22 Ordovician -1.03 Qingshuiquan, Qinghai Ultramafic 10 Ordovician -0.68 Anyemaqen, Qinghai Ultramafic 17 Ordovician -0.75 Donghe, Hubei Ultramafic 4 Ordovician -O.~ Dammgshan, GuangxI Maficvolcamc I OrdOVICIan -0.41 Dexmg, hangxI Maficvolcamc 2 OrdOVICian -0.84 lSoutheast Zhejlang Ultramafic 6 OrdOVICIan -O.~ FujIan Maficvolcamc 6 OrdOVICIan -O.~ Fujian Ultramafic 14 Ordovician -O.~ Guangdong Ultramafic 2 Ordovician -O.~ Hatnan Maficvolcamc I OrdOVICIan Stlunan O:~ Dabieshan Granitoid 2 515 4.41 Danfeng, NorthQmlIng AndeSIte 6 500=435 3.51 Helhe,NorthQmlIng AndeSIte 4 500=435 4.81 Erlangpmg, NorthQmlIng AndeSIte 3 500=435 4.51 Yunjiashan, NorthQinling Andesite 2 500-435 5 EastQinling,Henan Granitoid 7 485-455 2.71 Bao]l,ShaanxI RhyolIte 19 OrdOVICIan 7.11 SouthShaanxi Granitoid 7 Ordovician 5.31 Ylchun JIlIng, Hetlongjlang Granl101d 53 OrdOVICIan 6.~ Baiqing-Mishan Heilongjiang Granitoid 15 Ordovician 5 Bamalmlao-Barde Obo, DlOnte 13 OrdOVICIan 9.21 InnerMongolIal Huawendong, InnerMongolIa DlOnte 7 OrdOVICIan 6.~ JlshlShan, Qmghat Diorite 19 OrdOVICian 4.~ LajlShan, Qmghat Gramt01d 16 MlddldOrdOVICIan 5.51 Qaidanor, Qinghai Granitoid II 460 5.(1 NorthQilian,Gansu Andesite I LateOrdovician 4.41 Beishan,Gansu Diorite I Ordovician 7.51 Ylchun, HeIlongjIang RhyolIte 5 EarlyOrdovIcIan 61 XlaoHmgganlIng,Hetlongjlang RhyolIte 8 Early OrdovIcIan 6.11 XlaoHmgganlIng,HetlongjIang RhyolIte 80 MIddleOrdOVICIan 5.31 Ylchun, HeIlongjIang AndeSIte 23 MIddle OrdOVICIan 6.~ Jjljn Gabbro 6 Silurian -052 Jjljn Diorite 7 Silurian -065 AlxanObo,InnerMongolIa Ultramafic 7 ~417 O.~ Dengkou, InnerMongolIa Ultramafic 8 Stlunan 0.] XIaosongshan, InnerMongolIa Ultramafic 5 384 O.~ AlxaZUOgl, InnerMongolIa Maficvolcamc 12 385 O·G Altay, XmJlang Ultramafic 16 Sllunan 0.84 Altay, Xinjiang Ultramafic 2 408-396 -0.(1 Annanba, Gansu Ultramafic I Silurian -0.63 EastQiling,Henan Ultramafic 55 427-370 -O.~ Ankang Xunyang, ShaanxI Basalt 9 EarlySIIunan 0.45 AlxanObo,InnerMongolIa Granl101d 11 Sllunan 6.11 UlanObo,InnerMongolIa Gramt01d 8 Sllunan 6.G OaganNur,InnerMongolIa Gramt01d 6 Sllunan 5·G Sandaoqiao, InnerMongolia Granitoid 4 417 4.~ Jilantai,InnerMongolia Granitoid 11 Silurian 6.~ ~ppendlX 5 IntraplateDeformatIOn VelocIty of TectonicPenods In ChIneseContInentSInceMesoproterozoic 4I3

ContInuedl DeformatIon velocletyl IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) South Nigxia Granitoid 19 ~39l 4.71 Jjljn Granitoid 34 408 360 531 Kangbao,Hebel GramtOld I Silunan 4.81 Kangbao,Hebel DlOnte I Silunan 7.11 Dableshan GramtOld 4 426 4.71 Hmchlzl.,South ShaanxI GramtOld 40 Sllunan 6.11 Ankang-Xunyang,Shaanxi Rhyolite 4 Early Silurian 7.11 South Qilian, Qinghai Diorite 20 Silurian 6.71 Dangjinshan, Qinghai Granitoid 18 Silurian 6.51 Altay,Xinjiang Granitoid 34 408-396 8.51 East l unggar, XIjtang GramtOld 12 408-396 5.31 Altun, XInjiang GramtOld 5 ~400 5.81 hanshan, XInjiang GramtOld 12 ~400 5.71 WestKunlun,Xinjiang Granitoid 7 ~400 4.~ East Kunlun,Xinjiang Granitoid 5 ~400 5.~ East Qinling,Henan Granitoid 19 427-370 7 Fujian Granitoid 11 Silurian 5.~ ltanou, Fujtan GramtOld 5 Silunan 6.51 NInggang, llangxI GranItOId I Sllunan 5 Changtan,llangxI GramtOld 4 Sllunan 6.31 Wanz31, llangxI GramtOld 3 394 5.71 Lean, liangxi Granitoid 2 450 61 Xunwu,liangxi Granitoid 10 Silurian 5.~ Huhei Trachyte 15 Silurian 3.~ Hunan Granitoid 21 Silurian 7.11 Dongkou,Hunan GranItOId 12 421 360 7.\1 Hengshan,Hunan Granitoid I 364 5.~ Hainan Granitoid 19 Silurian 7.51 HaInan Rhyohte 2 Late Sllunan 8 Zhanxlan,Guangdong GranItOId 18 Silunan 7.31 Guangdong Rhyohte 19 Sllunan 6.51 WestGuangxi Granitoid 18 Silurian 7.71 Chenxi,Guangxi Keratophyre 2 Early Silurian 5 SoutheastGuangxi Granitoid 8 Silurian 6·41 NortheastGuangxi Granitoid 24 Silurian 61 ¥uIIn,GuangxI GramtOld 3 Silunan 6.11 lIngxI, GuangxI GranItOId I Sllunan 6.11 Wuzhou, GuangxI GramtOld I Sllunan 5.~ Lipu, Guangxi Granitoid 2 Silurian 7.~ lLillI

IAPpendix 5.4 Intraplate deformation velocity ofTianshanian Period(397-260Ma)

DeformatIOn velocletyl IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) XInk31IIng, HeilongjIang OphlOhte 12 Devoman O.~ BaogIng,HeilongJiang Ultramafic 22 Devoman 0.64 Hegenshan, InnerMongolia Ultramafic 18 Devonian -O.~ Badu, GuangxI Basalt Early Devoman 0.41 Wude, GuangxI Basalt MIddleDevoman 0.41 Napo, Guangxi Trachyte Late Devonian -0.21 fil4 Appendices

Contmued DeformatlOu velocletyl ( IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) Dakang,Fujian Ultramafic 2 350 -O.~ Sunke-Fulao, Heilongjiang Granitoid 13 322 5·11 Mudanjiang,Heilongjiang Granitoid 4 Devonian 7·11 Woduke-Meishan, Granitoid 5 Devonian 6.31 Inner Mongolial Dahelshan,Heilongjiang GranItOid 34 DevonIan 4·G Bikou, WestQinling Diorite I Devonian 4.7] Beishan,Gansu Rhyolite 2 Late Devonian 5.~ NorthQiadam,Qinghai Diorite 4 Devonian 5 South Qiadam,Qinghai Diorite 21 Devonian 5.51 !South QIadam,QmghaI GranItOid 9 DeVOnIan 6.~ Altay,XmjIang GranItOid II2 377 7.31 hanshan, XmjIang GranItOid 161 377 6·1 XmxmxIa, XmjIang GranItOid II 377 M East Kunlun,Xinjiang Granitoid 62 377 6.2 Dabieshan Granitoid 2 376-370 411 Jilm GranItOid 3 DeVOnIan 3.9 Olip, InnerMongolia Basalt 16 CarbonIferous 0.53 !Solon, InnerMongolia Ultramafic 22 CarbOnIferous 0.] Fujlan Basalt 6 E. CarbOnIferous 0.41 Jingxi, Guangxi Basalt I E. Carboniferous -0.41 LancangjiangPaleo-ocean Basalt E. Carboniferous -0.67 (after Mo XX] JinshajiangPaleo-ocean Basalt E. Carboniferous -0.9 (after Mo XX)I Duobaoshan, Heilongjiang Granitoid 38 Carboniferous 5 Jilm GranItOid 3 CarbOnIferous 4.31 JmgxI,Llaonmg GranItOid 6 312 6.31 Inner Mongolia(activearea) Diorite 8 Carboniferous 6.51 InnerMongolia(stablearea) DlOnte 4 CarbOnIferous 4.~ InnerMongolia(aclivearea) GranItOid 23 CarbOnIferous 6.51 Inner Mongolia(stablearea) GranItOid I3 CarbOnIferous 5·2 Belshan,Gansu Rhyolite I E. CarbOnIferous 7.] Beishan,Gansu Dacite I M. Carboniferous 4.7] Qilianxian,Gansu Diorite I Carboniferous 6.51 Xinxinxia,Tianshan Granitoid 174 ~ 300 62 NorthTianshan Granitoid 238 300-295 6.31 Altay,XmjIang GranItOid 160 300-295 6.11 WestJunggar GranItOid 126 300-295 5.~ East Junggar GranItOid 212 300-295 5.2 Guangdong GranItOid 5 CarbOnIferous 6.71 Guangxi Granitoid 8 Carboniferous 6.4 Piaotang,Jiangxi Quartz diorite I Carboniferous 5.S1 Laoheishan,Heilongjiang Basic volcanic 6 Early Permian -0.75 JIanpmg-XIfeng, LIaonmg Ultramafic 6 Early Permian 0.86 Qillanxlan,Gansu SerpenlinIte I Early Permian 0.79 JmgxI,GuangxI Diabase I Early Permian O.~ l'angma, GuangxI Basalt 3 Early Permian O·G Xichang,Sichuan Basalt 5 Late Permian -0.56 Dukou,Sichuan Basalt 7 Late Permian -0.41 Dongchuan, Yunnan Basalt 3 Late PennIan O.~ Lufeng, Yunnan Basalt 9 Late PennIan 0.21 WestGUlzhou Basalt 48 Late Permian 0.51 Border between Basalt IO Early Permian O·G Yunnan & Guangxj Lanpmg-Slmao, Yunnan Basalt 3 Early Permian -0.51 Ganzi-LitangPaleo-ocean Basalt E. Permian-E. Trias- -0.8 (after Mo XX)I sic ~ppendlX 5 Intraplate DeformatIOn VelocIty of Tectonic Penods InChInese ContInent SInceMesoproterozoic 4I5

ContInued DeformatIOn velocletyl ( IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) UIiji,Heilongjiang Granitoid 27 > 203 5.2 Sunke-Furao, Heilongjiang Grauitoid 103 Permian 5 BaoqIng-Mlshan, HeIlongJIang DacIte 7 EarlyPermian 7.2 Maanshan, HeilongjIang GramtOld 9 Early Permian 6.§ helI, HeIlongjiang GramtOld 47 EarlyPermian 4.~ Muhetun, HeIlongjIang GramtOld 41 EarlyPermian 6.31 Handagl, HeilongjIang GramtOld 2 310-308 5.71 SonglingArea,Heilongjiang Granitoid 33 EarlyPermian 4·71 Longzhen, Heilongjiang Granitoid 38 EarlyPermian 5.51 BaoqIng, HeIlongJIang GramtOld 14 EarlyPermian 7.31 Daluomlzhen, Heilongjiang GramtOld 36 Early Permian 5.31 BmxIan, HeIlongJiang GramtOld 58 EarlyPermian 4.2 MudanJlang, HeIlongJIang GramtOld 5 EarlyPermian 8.2 IShuangchengzl, HeIlongjIang GramtOld 51 Early PermIan 7.51 Wjn Dacite 62 permian 61 Jjljn Granitoid 232 302-254 551 TuleMod,InnerMongolia Granitoid II EarlyPermian 6.31 LlUjIayIngzl, InnerMongolIa GramtOld 5 Early Permian 7.§ Aohangl, InnerMongolIa GranItOId 4 EarlyPermian 5 lSandaoglao, InnerMongolIa GramtOld 10 288 279 6.71 InnerMongolIa (aclIve area) GramtOld 17 Early PermIan 5.2 InnerMongolia (stablearea) Granitoid 27 EarlyPermian 5.2 AlatanAbo,InnerMongolia Granitoid 12 289-252 7.71 Liaoning Granitoid 14 270-269 5.~ LiaonIng GramtOld 12 ~240 5.~ n6.5'E,41.7'N GramtOld 4 PermIan 5.31 1117.5°E,42.3°N Gramtoid I LatePenman 4.71 Kangbao-Weichang, Hebei Salicvolcanic 6 EarlyPermian 5·1 Kangbao- Welchang, Hebel GramtOld 20 266-250 4.71 Kangbao- Welchang, Hebel AndeSIte 13 266-250 4.2 Kangbao, Hebel GramtOld 20 266-250 4.71 IShanghuanggl, Hebel GramtOld 4 Early Permian 5.31 Qipanshan, Hebei Granitoid I EarlyPermian 4·71 SouthShaanxi Granitoid 7 EarlyPermian 7 Beishan,Gansu Andesite 1 EarlyPermian 5.<'1 Belshan,Gansu RhyolIte 2 LatePenman 7 Northern QaIdam, QInghaI GranItOId 5 EarlyPermian 6.] lSouthern QaIdam, QInghaI GramtOld 7 EarlyPermian 8 Gateof QaIdam, QInghaI GramtOld 2 Early PermIan 6.~ Southof EasternKunlun, Granitoid 6 259 5.\1 Fujian QuartzDiorite 6 EarlyPermian 7.4 Ganfang, Jiangxi Granitoid 1 Permian 61 YunkaIdashan, Guangdong SchISt I Early Permian 10 LIUZhou, GuangxI luff 1 Late Penman 8.71 Darongshan, GuangxI GramtOld 90 EarlyPermian 6.31 LanpIng-Slmao, Yunnan DaCite 4 Early PermIan 5.31 ~ ftl6 Appendlcesl Vtppendix 5.5 Intraplate deformation velocity ofIndosinian Period(260-200MaJI

DeformatIOn velocletyl - are extension, ea Rock Sample Periodor Age amount (Ma) others are shorten- mg)(cri17yr) BangongCo-Domar,Xizang Basalt 4 Early Triassic -0.21 East Hohxilshan Diabase 3 E &M Trjassic 021 Bayan Har Shan Basalt 6 E.&M. Triassic -1.21 IanggulaShan Basalt 8 E.&M. Inasslc -0.41 Paleo-JmshaJlang Ocean (Closmg) GranItOId E.Permlan- 4.69 (atter Mo XX) E:T.iJ.iiSSi.a North'I janshan (jumjtojd 61 ~219 471 Alatan Abo, 104.5°E, 40.3 ON GranItoId 25 ~ 235 5.81 Ela shan, Qinghai Acid volcanic 9 ~240 5.41 East Kunlun Granitoid 101 ~ 235 5.51 East Kunlun Acid volcanic 7 ~240 s.s Mmgshan LlXlan, GranItOId 132 ~ 233 5.~ NorthQmlmgl WestQmlmg RhyolIte 4 Early'InasSlc 6.81 NorthwestQiangtang Granitoid I 239.8 5.~ Baosahn,Yunnnan Granitoid 44 ~230 6.11 Lincang,Yunnan Granitoid 300 ~ 235 6.11 Nyalam-Yadong, Xizang Granitoid 1 235.8 5.51 Yarlung Zangbohang Basalt 7 Late Inasslc 0.21 Burang Daba Ophyohte 5 Late Inasslc I.G Altay,Xinjiang Granitoid 4 ~228 4.~ Hami, Xinjiang Granitoid 13 ~230 4.~ Raohe-Baoqing, Heilongjiang Ultramafic 81 Triassic -0.61 Wandashan, Heilongjiang Ultramafic 53 Late Triassic -0.48 Baoqing,Heilongjiang Acid volcanic 105 Late Triassic 5.51 HmgganlIng, HeIlongjIang GranItOId 355 ~229 4.~ rsn; HeIlongjIang 128.5°E, 47 ON GranItOId 47 Inasslc 4.81 liIin (jranjtojd 18 ~223 571 Hetao,InnerMongolia Granitoid 58 ~225 4.51 Jilantai, 105.5°E, 39.6 ON Granitoid 7 223 4.~ NQrthShanxj (iamjrQjd 12 ~227 B NortbHehei (jranjtojd IS ~226 5 West Shanxi Iliff 8 Triassic III Tianzhen-Yangyuan, Shanxi Nepheline-syenite 6 Triassic 1.51 Hezuo, NorthQinling Granitoid 75 ~227 6.~ Qmlmg GranItOId 213 ~226 5.51 Henan (iranitoid 6 ~224 4\1 Anhuj (iranitoid 12 no 230 551 JIangxI GranItOId 29 ~235 5.~ Hunan Granitoid 40 ~224 61 Zhuji, Zhejiang Granitoid 5 Triassic 4.81 Quxian,Zhejiang Granitoid 7 Triassic 5 Fujian Granitoid 13 ~226 5.§ GuangxI GranItOId 86 ~226 6.51 Guangdong GranItOId 12 ~225 5.11 Panzhlhua Xlchang GranItOId 15 ~230 6.31 Lancangjiang Paleo-ocean (clos- Granitoid ~230 5.3 (after Mo XX] ing) Jomda-Qamdo, Xizang Dacite 22 E. - M. Triassic 5.81 YalongJlang, WestSIchuan GranItOId 81 ~229 7 Dawu, WestSIchuan GranItOId 31 ~221 6.~ Lanpmg-Slmao, Yunnnan GranItOId III ~225 5.~ LaoyelIng, HeIlongjIang GranItOId 215 ~219 5.41 Dengkou, 106.5°E,40.7°N GranItOId 22 ~218 5.71 ~ppendlX 5 Intraplate DeformatIOn VelocIty of Tectonic Penods InChInese ContInent SInceMesoproterozoic 4I7I

ContInuedl DeformatIon velocletyl IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing)(cm/yr) Baotou,1I0'E, 40.3"N Gramtold I ~217 4.71 Liaoning Granitoid 51 ~213 5.41 Kuruktag, Xinjiang Granitoid 2 Triassic 6.~ SouthTianshan Granitoid 5 ~215 5.31 Qlmantag, Xljlang GranItOId 21 [nasslc 5.11 Qlmantag, Xljlang luff 2 ~211 5.81 KarakoDm Shan (jumjtojd 18 ~211 6~ Tianshui, northQinling Granitoid 101 ~217 5.41 south Qinling Granitoid 9 ~217 5.31 WestQinling,Qinghai Granitoid 15 ~219 6.~ Beishan,Gansu Granitoid 32 ~219 61 MIddle Qlhan GranItOId 75 ~218 5.51 Barkam, Sichuan GramtOld 70 ~219 6.51 Yldun, WestSIchuan Gramtold 45 ~218 7,;1 NorthQiangtang Diacite 2 LateTriassic 6.81 Yushu, Qinghai Acid volcanic 63 Late Triassic 5.51 Tanggulashan Acid volcanic 41 Late Triassic 5.31 lamantaweng Shan GramtOld 16 219.6 5.81 Jomda Markam, East XIzang ACid volcamc 50 Late [nasslc 7 Jomda Markam, East XIzang GramtOld 17 215 5.31 Ohjl, 104.5 'E, 41 ON GramtOld 3 ~203 5·G NorthBorderof Qaidam Granitoid 128 ~205 5.~ J;T84I f4ppendix 5.6 Intraplate deformation velocity of Yanshanian Period(200-135 Ma)

Deformation vclocictyl Sample Periodor Age ("-" is extension, IArea Rock amount (Ma) others are shorten- Ing)(cm/yr) East to Harbin Granitoid 56 ~ 170 5.71 NorthHingganling Granitoid 63 ~ 170 5.71 south HIngganhng GramtOld 19 ~ 166 5.~ Laoyehng GranItOId 86 ~ 167 4.71 liIin (jrnnjtojd 109 ~ 169 5 ~ Liaoning GramtOld 79 ~ 180 5 WestLiaoning Acid volcanic 137 M.&EJurassic 5.31 Chifeng Granitoid 6 169 3.51 Wuh31, InnerMongoha Syemte I 187 2.11 Nandahng FormtIon, Yanshan Basalt 21 ~ 178 4.~ haojlshan FormtlOn, Yanshan AndeSIte 30 ~ 165 4.51 Zhangjlakou FormtlOn, Yanshan Rhyohte 118 ~ 150 61 Helansban Granitoid 7 ~173 481 Shanxi Granitoid 73 ~ 170 41 Handan, Hebei Granitoid 16 ~ 148 5.21 East Shandong Granitoid 127 ~ 159 5.11 QInhng GramtOld 90 ~ 158 4.81 NorthHebel GranitoId 20 ~ 157 5 Southwest Henan (iranitoid 84 ~ 158 411 NorthHuaiyang Acid volcanic 7 > 144 4.71 Jlangsu GranItOId 2 JurassIc 4.\1 SouthAnhur GranitOId 52 ~ 153 5.71 Southeast Huhej (jrnnjtojd 199 ~ 166 5 II fil8 Appendices

Contmuedl DeformatIOn velocletyl IS extension, Area Rock Sample Periodor Age amount Ma others are shorten- ing) (cm/yr) WestZhejiang Rhyolite-andesite 7 ~ 190 6.~ NorthwestZhejiang Granitoid 108 ~ 157 5.31 East Zhejiang Granitoid 126 ~ 156 5.51 Fujlan Gramt01d 20 ~ 167 5.~ Fujlan Gramt01d 31 ~ 149 5.§ Jlangxl Gramt01d 24 ~ 190 5.~ JtangxI Gramt01d 38 ~ 164 6.31 Jiangxi Granitoid 25 ~ 148 5.71 Northeast Hunan Granitoid 21 ~ 161 651 MiddleHunan Granitoid 35 ~ 161 6.51 GuangxI Gramt01d 41 ~ 178 61 GuangxI Gramt01d 94 ~ 149 6.11 Guangdong Gramt01d 62 ~ 180 7.11 Guangdong Gramt01d 20 ~ 158 6.~ Guangdong Granitoid 183 ~ 144 6.~ SoutheastYunnan Granitoid 34 ~ 167 521 Tengchong, WestYunnan Granitoid 19 ~ 160 5.~ Panzhlhua Xlchang Gramt01d 9 ~ 167 4] Aba, WestSichuan Gramt01d 17 ~ 137.3 6.11 Markam, WestSIchuan Gramt01d 18 ~ 157 61 Dafu, WestSIchuan Gramt01d 35 ~ 154 5.71 Yalongjiang, WestSichuan Granitoid 5 ~ 187 6.~ Yidun,WestSichuan Granitoid 46 ~ 176 6.41 East Bayanhar, QmghaI ACid voIcamc 17 Early JurassIc 7.31 Bayanhar, QmghaI Gramt01d 21 ~ 192 61 QaIdam,QmghaI Gramt01d 29 ~ 152 6.11 Qaidamshan, Qinghai Granitoid 2 ~ 182 6·41 Northeast,Qinghai Granitoid 54 ~ 187 6.~ LangmusI, WestQmlmg Andesite 3 MiddleJurasSic 7.31 ltanshUl,North Qmhng Gramt01d 92 ~ 180 5.31 Altay Gramt01d 24 ~171 5.§ Altuo (jranitojd 1 Illrassic sa West Karakorum Dacite 3 ~ 167 62J Qarlong Baslte 6 E.&MJurassic -O.~ Qarlong Andesite 4 E.&M. Jurassic 5 Kunlun,Xljlang Gramt01d 11 JurassIc 6.4] NorthQIangtang Gramt01d I JurassIc 7 LumaCo - Doma, XIzang Gramt01d 8 ~ 167 6.4] Jomda, Xizang Gramt01d 4 ~ 143 6.31 Qiangtang-Qamdo,Xizang Rhyolite-andesite 8 Jurassic 5·41 Tanggula, Xizang Granitoid 4 Jurassic 6.31 Amdo-Nyainrong,Xizang Granitoid 10 ~ 163 5.51 Naggqu Barle,Xizang Ophyohte 1 Late JurassIc l.5I Bangongco NUllang, XIzang Ophyohte 81 Late JurassIc 4 Bangongco Dengqen, XIzang Ophyohte 64 JurassIc 1.1 Bangongco-Dengqen, Xizang Basalt 17 Jurassic 4.31 Ngari, Xizang Granitoid 13 ~ 165 6·41 North Nyainqentanglha Xizang Basalt 8 M.&L.Jurassic -0.41 North Nyainqentanglha Xizang dacite 54 M.&L. Jurassic 6.~ !Shlquanhe, XIzang Ophyohte II M.&L.JurassIc 3.21 !South NyaInqentanglha XIzang daCIte 6 M.&L. JurassIc 61 LagUlgangn, XIzang Basalt 5 M.&L. JurassIc 0.41 2,9841 ~ppendlX 5 IntraplateDeformatIOn VelocIty of TectonicPenods In ChIneseContInentSInceMesoproterozoic 4I~

VtPPendix 5.7 Intraplatedeformation velocityof Sichuanian Period (135-56 MaJI

[?eformationvelociety ("-" is extension'l ~rea Rock Sample Periodor Age amount (Ma) others are shorten- jng) (clriJyr~ ISE YarlungZangboJiang Basalt 18 EarlyCretaceous -0.7 ISW Yarlung ZangboJiang Basalt 88 Early Cretaceous -0.5 Ngan-Shlquanhe, Xizang Basalt 13 EarlyCretaceous 0.9 Ngari-Rutog, Xizang Basalt 6 Early Cretaceous -0.5 East NyaIngentangulha GramtOld 25 ~ 128 6.5 Luobusha, XIzang Ophyohte 85 Cretaceous -3.3 Cogen-Namco, Xizang Ophyolite 20 Cretaceous -3.11 lSouth Yarlung ZangboJIang Gabbro 5 Late Cretaceous -1.8 Yamzho Yumco DIabase I Late Cretaceous -1.11 Yarlung ZangboJIang Gabbro 7 Late Cretaceous -0.3 Yarlung ZangbolIang DacIte 24 Late Cretaceous 5.1 Yangbajing, Xizang Granitoid 49 ~76 (1 Nyainqentangulha Dacite 78 Late Cretaceous- 5.~ Eocene WestLancangjiang Granitoid 1 ~76 6.1 North Nyamgentangulha GramtOld 18 ~ 104 5.§ Ngan Shlguanhe,Xizang AndeSIte 31 Late Cretaceous 5.~ Eocene IShiguanhe-Bomi Granitoid 8 ~ 108 6.5 Gegyai,Ngari Dacite 25 Late Cretaceous- 5.5 ~ WestQiangtang Granitoid 1 ~ 9004 6·41 g2°E,36°N Basalt 2 Paleocene-Eocene -0.3 79°E,35°N Dacite I Late Cretaceous 6.(j KarakomID Granitoid 10 ~95 641 Tanggula, Qinghai Basalt 12 Cretaceous 4.~ Tanggula, Qinghai Granitoid 8 ~85 5.5 Tongren, Qinghai Basalt 2 Cretaceous -0.5 Jiuquan,Gansu Latite 5 83 2.71 Garze-Lltang Paleo-ocean (cios- GramtOld 42 Cretaceous 6.~ ii1g} Bj IllOXlJeshan (jranjtojd 14 1011 52 6~ NujiangPaleoocean(c1osing) Granitoid 78 138-51 6·41 Dawu, WestSichuan Granitoid 18 139-52 6.5 Panzhihua-Xichang Granitoid 14 ~ 123 5.'1 SoutheastYunnan Granitoid 162 102-78 5.3 GuangxI GramtOld 143 132-68 § lSoutheast GuangxI ACId volcamc 66 100-67 4.~ Guangdong GramtOld 123 135-90 5.71 Guangdong Granitoid 84 90-55 5.'1 Hunan Granitoid 10 131---fi5 641 Jiangxi Granitoid 19 135-70 5.81 Fujian Granitoid 187 127-70 6.1 Fujlan ACId volcamc 475 127 125 § Zhellang GramtOld 22 125 70 5.3 IShanghaI ACid volcamc 42 136 84 4.§ Nanjing-Wuhu Granitoid 41 137-91 5.~ South Anhui Granitoid 14 136 115 5 1 Lujiang-Zongyang,Anhui Acid volcanic 62 133-108 3.(1 Dabie-Qinling Granitoid 98 121-105 § SoutheastRubel ACId volcamc 153 132 102 4.1l Henan Acidvolcanic 218 115 87 481 fi20 Appendices

Contmuedl peformatlOnveloclety IS extension, rea Rock Sample Periodor Age amount Ma others are shorten- ling) (cm/yr] South Gansu, Tuff 3 LateCretaceous 5.(j Tianshui, NorthQinling Granitoid II 127-104 5.3 Mingshan-Lixian, Granitoid 5 Cretaceous 5.3 NorthQmlmgl Helanshan ACId volcamc 27 7Pi6 41 ~ 04.5' E, 40.3' N Basalt 1 LateCretaceous 41 ~04.5'E, 41'N ACId volcamc 23 EarlyCretaceous 4.71 Shanxi Granjtoid 23 135-74 541 Handan,Hebei Alkalirock 6 110-52 2.71 WestShandong ACId volcamc 337 133-78 4.71 East Shandong ACId volcamc 285 136-90 5.71 Yanshan GramtOld 52 140-110 3.41 WestLlaonmg ACId volcamc 369 135-70 4.~ LIaonmg ACId volcamc 74 135-70 51 Liaoning Granitoid 70 132-S0 4.~ Jjljn Granjtoid 34 104-76 51 south HmgganIrng GramtOld 74 132 91 4.~ LaoyeIrng GramtOld 18 128 76 77 NorthHmgganIrng GramtOld 30 132 105 5.~ JapanSea RhyoIrte 11 127 5.1 WestPacificOcean 90-S0 Magneticanomalies, SI Em[!

Vtppendix 5.8 Intraplate deformation velocity ofNorth Sinian Period(56-23 Ma]

Deformation velocietyl ("-" is extension, ~rea Rock Sample Periodor Age amount (Ma) others are shorten- mg) (clriJyr) WestPacific Ocean 40-30 Magnetic anomalies, 9 Baitoushan, Jilin Trachyte-rhyolite I Eocene-Oligocene 5.4 JIIrn Basalt 7 32.9 4.2 LowerLlaohe Basalt 54 Eocene=OIrgocene 3.2 Hebei Plain Basalt 26 49-17 54 Fansi,Shanxi Basalt 2 Eocene-Oligocene 4·2 MOJlth of Yellow Rjver Basalt 6 45-19 64 SouthHuanghai-NorthJiangsu Basalt S 47-42 4.2 NorthAnhui Basalt 4 Eocene-Oligocene 5.~ Hefei,Anhui Basalt 4 Eocene-Oligocene 5.4 SoutheastHubel Basalt 2 52 41 South AnhUl Basalt 1 42.6 2.2 CoastalMountians, Taiwan Basalt 20 Paleogene 7.] Fujian Basalt IO Paleogene 3.~ Jiangxi Basalt 2 32-20 5.4 Sanshui,Guangdong Basalt 7 51-45 3.31 GuangxI Basalt 4 47 33 3 EasternNanhar 52 25 MagnettcanomaIres, 4.~ Jmshajlang Red RIver 44=23 SlmstralsIrp,0.451 MjddleYllOnan Basalt 9 52 14 2\1 West Yunnan Basalt 2 18 6B Panzhlhua Xlchang Basalt 2 31 1.2 Jomda-Yulong GramtOld 128 55 34 5.71 Tianshan Granitoid I Paleogene 3 ~ppendlX 5 Intraplate DeformatIOn VelocIty of Tectonic Penods InChInese ContInent SInceMesoproterozoic 421

DeformatIOn velocletyl Sample Periodor Age ( IS extension, rea Rock amount Ma others are shorten- ing) (cm/yr) NorthTanggula Granitoid 17 46-36 4.51 SouthYushu area Trachyandensite 19 Paleogene 0.75 WestKarakorum Granitoid I 33.6 4.51 NyaInqentanglha GramtOld 53-31 5.~ Nyamqentanglha DacIte 17 Ohgocene 5.4 Yamzho Yumco (NWW) Dl3base 3 Paleogene 1.1 Yarlung ZangboPaleo-ocean GramtOld 43-32 6.31 (closing] Eastend of Himalaya Shan Basalt 10 Eocene -0.21 TIl Sources of rock chemIstry data: Data of Lower Ll3ohe, Mouth of Yellow RIver and Imwan, after E ML and Zhao DS(1987); Panzhihua and Xichang, after LuoYN (1985); Jinshajiang-Red River, after WuHW (1989);Nanhai, after Liu ZS (1988); JapanSea, after Uyedaet aI., (1974); Data of West Yunnan are sent byProf.Zhao CH (personal commumca­ tIon); otherscollectedfromgeological survey.

Vtppendix 5.9 Intraplate deformation velocity ofHimalayan Period(23-0.78 Ma)

DefonnatlOn velocletyl IS extension Area Rock Sample Periodor Age amount (Ma) others are shorten mg) (clri7yr) IZayu, Southeast Xizang Granitoid 16 20-16 6 IHigh Himalaya Granitoid 30 21-10 5.~ Nyainqentanglha Granitoid 19 23-12 6 IN yaInqentanglha DaCIte 6 Neogene 5.] Qamdo,XIZang DaCIte 2 Neogene 6 QIangtang DaCIte 31 Neogene 5.61 90'E,34.6'N AndeSIte 25 Neogene 4.91 90'E,36'N Trachyandenslte 9 Neogene 5.1 86.s'E,36'N Dacite 6 Neogene 4.~ 82°E,36°N Trachyandensite 13 28-20 4.41 175°E, 38.5'N Trachyandensite 13 1.4-1.2 4.1 IWest Karakomm {Jnwitojd 1 17 10 491 87'E, 36.3'N AndeSIte 15 10.5 5 4.] ITanggula Shan Rhyohte 14 26=10 4.] IUrad Houqi Basalt 1 1.19 -OJ IXilingol Meng Basalt 36 ~14 -0.141 NorthwestShanxi Basalt 21 26-7 -0.241 IHannuoba, Hebel Basalt 72 ~18 0.231 IWest Henan Basalt 2 11 3.5 0.151 IMudanj13ng Basalt 11 16=1.1 0.531 INearby Changb31shan Basalt 154 14=1.2 0.21 lEast Liaodong Basalt 6 9.8-0.9 -0.2~ Shandong Basalt 86 21-0.86 -0.281 [Iancheng-Lujiang fault Basalt 85 16.5-9 -0.251 lEast Yunnnan Basalt 18 Neogene 0.331 Southeast GuangxI Basalt 7 Neogene 0.341 IBmyu, SIchuan Basalt 3 Neogene 0.231 ITengchong, Yunnan Basalt 5 23-2 -0.371 [Iengchong, Yunnan Basalt 13 2-0.78 5.61 IMlddle Zhejl3ng Basalt 50 Phocene -0.251 !West Fujl3n Basalt 37 Neogene -0.141 fi22 Appendices

DeformatIOn velocletyl ( • IS extension Area Rock Sample Periodor Age amount Ma others are shorten ing) (cm/yr) Coastal area of Fujian & Basalt 128 20-1.8 -0.431 Guangdong Oceancrust of Japan Sea Basalt 7-1.8 -0.351 IWest Honshu,Japan Basalt 2 6=0.8 0.2~ IRyukyu Irough Basalt 2 11-1 0.91 lEast I ajwan rift Basalt 66 25-1 85 () 681 Ipenbu Islands Basalt 48 ~2 -0471 117.5'E, 17.5ON Basalt 14.1 -0631 Basalt 3.49 -0.281 IPhIllppme Sea Plate 17 MagnetIc anomalIes, 8 IPhllIppme Sea Plate 4 MagneticanomalIes, 4 11,07(1 Sourcesof rock chemistrydata:Data of FujIan,Guangdong, 131wan, Iancheng-Lujlang,after E ML and Zhao DS (l987)j Changbmshan, after Jm BL et aI., (1994); Nanhm,after Lm ZS (1988);Japan Sea, after Harumoto(1970), AokI (l987)j IXilingol, after Chi JS et al.,(l988); Tengchong, after Liao ZJ (1988);Penghu Islands,after Chen (1973); RyukyuTroughj after Liu CB (1989),PhilippineSeaPlate,afterSenoandMaruyama(1977, 1984);otherscollectedfromgeological survey. f4ppendix 5.10 Intraplatedeformation velocityofNeotectonic Period(since 0.781 IMUJ

IDeformatlOn velocletyl ("-" is extensiOnj ~rea Rock Sample Periodor Age amount (Ma) others are shorten ling) (cmlyr) North QIangtang lrachyte-andeslte 7 0.067 4.51 ~7' E, 36J'N Trachyte 2 Late Pleistocene ~ 75 °E, 38.5'N Irachyte-andeslte I Late Pleistocene ~ ~1.6°E, 35.8°N Rhyolite 3 Holocene 4.4 Tengchong, Yunnan AndeSite-basalt 26 Late Pleistocene & 4.~ Holocene QiongshanHainan Basalt 3 0.319 -0.5 I ejzhoJl penjnsula Basalt 36 Holocene () 61 Nvshan Fushan, AnhUi Basalt 16 0.73~0.5 0.18 Hannuoba-Datong,ShanXI Basalt 72 0.73~0.2 0.18 LowerLlaohe, Llaomng Basalt 14 0.12 0.16 Changbaishan Trachyte 69 Mid-Late 3 Ipleistocene Changbaishan Trachyte 21 Holocene 2.~ Longgang,Jilin Basalt 31 0.07 -0.14 Wudalianchi, Heilongjiang Basalt 113 0.39 -0.12 Mudanjlang, HeIlongjIang Basalt IS Mid Pleistocene 0.211 1H010cene Daxiongshan,Heilongjiang Basalt 10 Mid Pleistocene- -0.5 1H010cene Hakone,Japan Irachyte-andesne I Holocene 'J RyukyuTrough Rhyolite 6 Mid Pleistocene- 5.2 1H010cene Datun,Taiwan Andesite 9 Mid Pleistocene- 8.) ~

Sources of rock chemistry data: Data of Taiwan, after E ML and Zhao OS (1987); Tengchong, after Liao ZJ (l988)j Changbaishan, after Jin BL et aI., (1994); Nanhai,after Liu ZS (1988);Japan Sea, after Harumoto (1970),Aoki (l987)j XIlmgol,after Chi JS et aI., (1988);Ryukyu lrough, after Lm CB (1989),PhllIppmeSea Plate, after Seno and Maruyama (1977, 1984);otherscollectedfromgeologicalsurveyJ ~eferences for Appendix 5 423

VtPPendix 5.11 Plate deformation velocitY (cmlyr)in recent, accordingto the data of GPS (362 stations)and earthquake moment (after ZhangPZ e~ al.,2002)

IArea DeformatiOn velocity Area DeformatiOn velocity IIndlan Plate 4.1 Ordos 0.81 IHlgh Himalaya 1.5 NorthChma 0.3 Gandlse 2.85 Yanshan WestLIaomng 0.451 lEast Qiangtang 2.8 NortheastChma 0.351 BayanharShan 2.1 North Northeast China O.O~ QaIdam 1.3 NorthJiangsu 0.7 IAltun 0.8 Kazakhstan 0.41 INorth QIlIan I ShanghaI 1.1 IWestTorim 11 Sichuan Yunnan 11 IWest hanshan 2 Baoshan, WestYunnan 0.551 Middle Tianshan 07 Red Rjver 071 Bogda Shan,Xinjiang 0.2 Xiaojiang, WestSichuan 1.251 IWest Junggar 0.1 East Yunnan 0.'1 IAltay, Xmjlang 0.22 SouthChma IAlxa 0.5 PhllippmeSea Plate 4.1

IReferences for Appendix 5

~oki K(1970)JapaneseIslandarc:Xenolithsin alkalibasalts,high-alumina basaltsandcalc-alkaline andesitesanddecites. In: NixonPH (ed) MantleXenoliths. pp.319-334.John WIley & Sons,New York. ~ureau of Geologyand MmeralResources of Provmces (1984 1993)RegiOnal Geologyof Provmces. Geological Pub-I lishmgHouse,Beljmg(m ChmeseWith Englishabstract,as shownm References for Chapter 1).1 K:hl JS (chiefeditor)(1988)The Studyof CenozOIc Basaltsand UpperMantleBeneathEasternChma (Attachment KlmJ berlites).277pp.ChinaUniversity of Geosciences Press,Wuhan (in ChinesewithEnglishabstract).1 '" ML, Zhao DS (1987)The CenozoicBasaltsand Deep-derived RockXenolithsof EasternChina.490pp.SciencePress, Beijing(in Chinese). HarumotoA (1970)Volcanic rocksand associated rocksofUtsuryoto Island(JapanSea).Geol. Surv.Japan, 15.1 gmBL,ZhangXY(1994)Researchon Volcamc Geologyof ChangbalMountams. 223pp.Northeastern Korean NatiOnalityl EducalionPublishmgHouse, Yanll (m Chmese). [:IaoZJ (1988)Late CenozOIc Volcano ofTengchong. In:TongW,ZhangMT,Geothermal ofTengchong, pp.I-19. SClencij Press,Beijing(in Chinese). Liu CB (1989)The pumicein Okinawatrough.ActaPetrological et Mineralogical 8(3): 193-202(in Chinesewith Englishl abstract).1 ISeno I (1977) Ihe mstantaneous rotauon vectorof the PhllippmeSea Platerelativeto the EuraSian Plate. Iectonophyslcsl 42(2-4): 209-226. ISeno I, MaruyamaS (1984)Paleogeographic reconstructiOn and ongm of the PhIllppme Sea. Iectonophyslcs 102(1=4): :rr::8'[ ghang PZ, WangQ, Ma ZJ (2002) GPS velocityfieldand activecrustal blocks of contemporary tectonicdeformation irj continental China.EarthScienceFrontiers9(2):430-441 (in ChinesewithEnglishabstractj] fi24 Appendices k\ppendix 6 Paleomagnetic Dataof Chinese Continent and Its Adjacent Are~

IStratasymbols refer to that of mtematlOnal stratigraphic chart (UNESCO and lOGS, 2000); N IS the amount of samples orl Isitesused in statistical analysis; I/Jp(O) are the degrees of longitude of virtual geomagnetic pole; Ap(') are the degrees o~ Inorthlatitude of VirtUal geomagnetiCpole ("-" IS south latitude); fX<)s IS radms (degrees) of mcle of 95% confidence abou! !he mean direction; Dn is mean paleomagnetic declination in degree; pnis mean north paleolatitude in degree ("-" i@ Isouth latitude). The data of D and P recalculated according to central reference point of block, based on the original datal [rom sources. The symbols of plates or blocks are the same as in the paleotectonic reconstruction figures.

1. Sino-Korean Plate (SK) (central reference point: before Late Jurassic is 1l2°E, 38'1'1;after Early Cretaceous is 115°E, 37°1'1)

Q 25-0Ma 8 25.2 84.9 4 353.6 36.8 Lm C et a!., 1983 II' 23-2.6 9 208 86.2 4.4 4.7 36.7 Lm JL et a!., 1985; Cheng GL et a1., lY\l~ E 65-24 4 203.5 79.7 9.1 12.9 36.6 Cheng GL et a!., 199~ IK2 100 66 I 170.7 79.6 5.5 11.6 42.3 Zheng Z & Kono, 19911 IK I 137-101 I 210.8 75.9 9.7 17.1 34.3 Ma XH et a!., 1993 h 165 137 2 221.8 69.4 15.4 22.2 28 Fang OJ et a!., 1988 Jz 190-166 5 229.7 76.8 5.6 3.6 31 Ma XH et a!., 1993; Cheng GL et al., 19881 J1201 191 1 286 82.4 6.8 0.9 30.4 MaXH eta!., 1993 '13 227 - 206 I 7.7 62.3 3.8 30 27 Ma XH et a!., 1993 12241-2287 2 61 2.9 330.1 24.1 Fang OJ eta!., 1988; MaXHetaI., 199.J T1250-242 6353.756.94.6 329.6 18.2 FangDJetal.,1988;MaXHetal.,199~ P2277-211 II 355.1 50.3 5.7 324 14.2 Zhao XX et a!., 1990; Ma XH et a!., 199~ PI 295-278 I 359.2 47 4.5 319.7 13.9 Ma XH et a!., 1993 C 354-296 3 333.3 56.5 6 338.2 10.8 Lin JL et al., 1985; Wu HN, 1991 PI-2490-455 6 323.4 33.4 8.5 333.5 12.9 Huang BC et a!., 1999; YangZY et a!., 199~ E3500-491 II 323 28.3 7.3 331.6 -17.6 Huang BC eta!., 1999; E2513-501 17 324.1 30.6 7.4 331.7 15.1 Huang BC et a!., 1999; E1543-514 8 332.4 20.6 10.3 319.7 202 Huang BC et a!., 1999; North Korean Peninsula (KN) (central reference point: 128°E,41°N) Q 1 335.3 85.2 4.3 357.5 36.5 SasaJlma, 1981 1 26 75.6 7.1 342.2 36.5 Sasajlma, 1981 I 315.9 81.8 4.4 358.9 33.3 Sasajima,1981 7 194.9 66.5 9.8 30.9 43.4 Sasajima, 1981 ~I 2 205.7 22.6 10 77.7 21.5 SasaJlma,1981 4 212.9 54.4 17.4 43.5 34.9 Sasajlma, 1981 South Korean Peninsula (KS) (central reference point: 128°E, 36°N) IK2-365-90 1 191 69 8 25.8 42.9 Vander Voo, 1993 IK65-144 1 195 64 6 32.8 41.8 Vander Voo, 1993 K1 98 144 I 183 76 3 15.7 43 Van der Voo, 1993 J 144-178 1 174 63 9 31.2 51.2 VanderVoo,1993 J 133-178 1 176 63 9 31.9 50.3 Kim & Van der Voo, 19901 J 157-202 1 213 54 17 43.2 31.1 Kim & Vander Voo, 19901 T 708 245 I 216 34 15 63 21 Kim & Van der Voo, 19901

2. Yangtze Plate (YZ) [central reference pomt: before Jurassic IS IOS'E, .lOON; after Early Cretaceous IS 106.5°E, 29.5°N~ Q 2 I-OM, 4 222.6 87.5 11.3 2.6 28.4 Zhm yJ, 1989 N 23 26 8 18.8 85.7 9.8 355.1 29.6 Liu C, 1976; Lin JL, 1987 E 65-24 8 200.2 81.1 7.5 10 28.5 Li HM et a!., 1965; Liang QZ, 1986; Zhuang iZI1,T988 IK2100-66 4 185.4 75.1 5.9 17.2 31.3 Kent et a!., 1986; Huang KN et al., 1993j Zbu ZW et a!., 198~ ~ppendlX 6 PaleomagnetIc Data of ChmeseContmentand Its Adpcent Area 425

Conti.nuedJ ~trata N pp(O) Ap(O) CX95 D(O) P(O) Source@ IK t t37 101 4 219.3 77.1 5 13 23.9 Kent et aI., 1986; Huang KN et aI., 1993j IZhu ZW et aI., 198~ 1} 16S-13S 2 214.9 65.7 9.1 24.2 19.5 Liang QZ, 1990;Cheng GL, 199<'1 J2190 166 5 205.7 70.8 7.6 20.9 24.8 Liang QZ, 1990;Zhu ZW et aI., 1988;Enkinl let aI., 1992a J1205-191 1 190.9 65.5 5.3 28.1 28.7 Huang KN et al., 19931 '13227 206 23 190.2 55.8 6.5 39 27 LIangQZ, 1990;ZhuZWet aI., 1988;Cheng IGL et aI., 1996;Zhou YX et aI., 1988 T2241-228 4 228.6 69.8 16.8 17.6 17.7 Zhu ZW et aI., 1988;Opdyke et aI., 1986j IChan et al., 19841 '1I 250-242 9 218.3 52 5.6 35.1 10.6 Enkm et aI., 1992; Zhu ZW et aI., 1988j ppdyke et aI., 1986

P2257-251 13 243.6 55.3 5.2 22.1 2.4 Lm C, 1987;Zhao XX et aI., 1996; WU HNI let aI., 1999;Huang KN, 1986;Ma XH et al.J isss PI 295-258 228.8 48.7 12.3 33.3 3.3 WuHN et aI., 1999;Liu BJ et aI., 1993 C2-3320-296 229.9 53.5 24 29.4 6.2 Zhang SH et aI., 20011 IC I354-321 229.1 47.5 9.6 34 2.3 Zhang SH et aI., 200II l)3372-355 234.1 45.4 6.6 33 -1.6 Zhang SH et al., 200~ DI-241O-373 231.4 36.1 12.1 40.9 6.9 Zhang SH et aI., 200~ S2-3420-411 195.7 6.8 5.3 83.8 2.8 Opdykeet aI., 1987 SI 2438 420 157 55.7 7.9 153.5 6.5 WuHN et aI., 199~ PI 2490 460 154.9 -38.4 13.7 144.6 -8.8 WuHN et al., 199~ E2513-500 185.1 39.5 7.8 129.1 11.7 BaJLX et aI., 199~

3. Cathaysian Plate (CA) (centralreferencepoint: 1I3.6°E, 25°Nj 111 I 209.2 I 9.1 88.5 5.5 ChenHH et aI., 19911 Cl I 227.7 22.6 19.7 58.9 10.3 ChenHH et aI., 19911 01 1 351.1 33.5 10.4 314.4 -10 ChenHH et al., 19911 D2 1 205.4 -24.9 14.8 111.2 -11.8 ChenHH et aI., 19911 ~3 1 54.5 -65.5 6.1 201.3 -11 Lm BJ et aI., 199~ ~2 I 51.5 -65.5 4.8 202 -12 Lm BJ et aI., 199~ reI 1 49.8 -62.2 8.4 205.4 -10.8 Liu BJ et al., 199~ IlaJwan block (TW) (centralreferencepomt: 121.5'E, 23SN) 11-5Ma 1 256 82 8 6 17.8 Vander Voo,1993 15-24Ma 1 294 82 13 1.1 15.6 Vander Voo,1993 N: -Ni 8 268.9 65.9 10.8 12.7 2.8 Li OG et aI., 1991

~. Blocksin the Hingganling-Mongolia collisionzone (XM) ~I 2 358 81.6 4.8 349.7 44.3 Manzhouli, 117°E,48.9°N; Zhao XX et al.j f990 1] 7 192.6 69.2 4.4 31.3 50.2 Huaan, 123.1°E,47°N; Zhao XXetal., 19901 1] 2 185 56 7.8 49.2 47.5 Balm ZUOgl, 1I8.9°E, 43.8°N; Zhao XX ej lal.,1990 I' 7 47.7 84.5 4.9 353.1 43 Jmmg, 113.2°E, 40.9°N; Zhao XX et al.J 19'1ll f2 4 56.7 -8 7.1 244.4 13.7 Balm ZUOgl, 1I8.9°E, 43.8°N; Zhao XX ej lal.,1990 f2 7 327.5 63.5 8.2 347 18.6 Wudan, 118.9°E, 42.7°N; Zhao XX et sn 19'1ll C3 31.6 77.7 6.6 343 43.1 Balm ZUOgl, 118.9'E, 43.8' N; Zhao XX ej lal.,1990 f1"26 Appendlcesl

Conti.nuedI ~trata N pp(O) Ap(O) CX95 D(O) P(O) Source@ (:, 4 304.5 77 5.5 358.7 36.2 Hailar, 119.8°E, 49.2°N; Zhao XX et al.J l'l2O (:2 231.2 46.9 8.9 43.7 23 Ming'an Obo, 113.2°E, 43.1°N;ZhaoXX e~ rar,T99Q Wandashan block(ND) (central reference point:133°E,46.3°N) IKI 1 224.1 51 2.9 49.1 33.6 ShaoJAet aI., 19911 11 3 1 47 0.4 5 266.8 2.5 ShaoJAet aI., 199~ "'I 1 214.1 -22.6 4.1 112 -10.3 ShaoJAet aI., 1991 K:3 1 251.6 0 23.2 68.5 19.4 ShaoJAet aI., 19911 JIamUSI block(JM) (central reference pomt:QIlathe, 131.1°E, 45.8°N) 1K2 1 57.9 79.3 12.1 344.6 48.2 ZhangSH, 1996 [(I 1 63.7 64.4 5 322 49.7 ZhangSR, 1996 h 1 59.6 71.3 15.7 332.7 48.6 ZhangSR, 1996 ~agan block(YO) (central reference point:102.6°E,41.7°N) fl 1 246.8 64.3 9.5 15.6 19.7 Zhu H et aI., 19871 10 1 296 65.3 10.2 354.1 17.5 ZhuR et aI., 19871 IS3 1 205.9 -25.7 12.4 102 -26.4 Zhu H et aI., 1987, Polarre-correctionl 03 1 216.1 -17.8 7.1 88.4 -29.1 Zhu H et aI., 1987, Polarre-correctionl ~3 1 206.6 -15.7 4.1 92.9 -20.7 Zhu H et aI., 1987, Polarre-correctlOnl

s, Siberian Plate (SB) (central reference point:80GE, 60GNj Q2Ma 13 157 86 4 8 60.1 Khramov et aI., 198~ Nz5 5 152 83 3 14 61.4 Khramov et aI., 198~ NI15 9 156 80 7 22 60.9 Khramov et aI., 1981 ~325 3 I37 72 14 38 65.2 Khramov et aI., 19811 EI 245 19 161 76 3 28 59.2 Khramov et aI., 198~ K365 3 152 74 13 33 61.1 Khramov et aI., 198~ K2100 6 167.4 69.5 8.7 38 55 Khramov et aI., 1981 K1121 5 166 70 4 37 55.7 Khramov et aI., 198~ IJ3142 6 150 70 9 41.1 60.7 Khramov et aI., 19811 IJ z J73 6 132 63 11 60.4 65.7 Khramov et aI., 198~ IJ1 195 4 130 69 15 46 67.5 Khramov et aI., 19811 T3207 6 129 56 8 77.3 64.2 Khramov et aI., 1981 T2238 7 150 52 7 69.9 52 Khramov et aI., 19811 11 245 9 156 52 4 66.1 49.2 Khramov et aI., 19811 lP2253 6 161 42 7 72.3 39.6 Khramov et aI., 198~ WI 268 5 159 38 9 77.1 37.5 Khramov et aI., 1981 C3288 5 158 34 11 80.9 34.8 Khramov et aI., 198~ D 360 7 151 28 8 91 33.4 Khramov et aI., 19811 S 420 8 121 4 19 136.4 18.4 Khramov et aI., 19811 02460 11 130 -22 4 134.7 -1.5 Khramov et aI., 1981

0 1 490 12 132 -40 7 14Q.4 -18.7 Khramov et aI., 19811 IE1530 4 157 44 12 124.8 31.4 Khramov et aI., 198~

~. Junggar Plate(JG) (central reference point:86°E, 46°Nj K 83 -14.1 183.4 29.8 n YA et aI., 199~ IT 180.5 59.3 17.9 39.1 36.2 Li YAet al., 1992 l' 179.2 45.3 27.7 52.7 28.2 n YA et aI., 199~ P 175.6 40.9 27.4 59.4 28.3 Li YAet al., 1992 C 200.6 59.5 11 31.6 28.2 n YA et aI., 19921 ID 312.4 68.7 25 342.4 29.7 Li YAet al., 1992 ~ppendlX 6 PaleomagnetIc Dataat ChmeseContment and Its Adpcent Area 4271

~trata N pp(O) Ap(O) CX95 D(O) P(O) Source@ S 17.5 -60.8 18.6 211.7 -30.2 LI YA et aI., 19921

7. Kazakstan Plate(KZ) (central reference point 77°E,500Nj IEl 2 269 78 6 357 38.2 Khramov et aI., 198! lEI 2 196 76 11 16 41.3 Khramov et aI., 1981 ~2 4 180.2 68.4 16 28 41.2 Khramov et aI., 1981 [(1 2 192.5 65 4 28 35.3 Khramov et aI., 1981 JI-2 3 233.2 62.5 19 12 24.1 Khramov et al., 19811 IT I 2 323.5 32 II 308 10.9 Khramov et al., 19811

~. XiyuPlate(XY) KlJ 1anm block(IR) (central reterencepomt 83°E,39.5°N)

N 2QMa 3 268.3 79.2 1.5 358.9 28.9 Li YAet al., 1989 IE 40 3 223.7 75.5 10.6 10.3 27.8 LIYA et aI., 1989 KIDS 1 211.6 69.7 8 17.5 25.4 LI YPet aI., 1988 K 134 3 217.1 68.1 15.7 16.9 22.9 LI YP et aI., 1988;Meng ZF, 1990;Zhang ZK, 1989 J 150 1 219.9 65.6 14 17.5 20.3 Li et al., 198\! J 172 I 185.9 62.7 13.5 30.8 29.1 FangOJ et aI., 19921 [I' 238 4 181.5 63.7 10.7 30.9 31.3 FangOJ et al., 1992;Li YAet al., 19851 IP 250 4 193.1 70.8 6.3 21.1 30.9 FangDJet aI., 1992;Bm YHet aI., 1985 ~ 306 5 17l.3 51.9 9 46 31 FangOJ et al., 19921 0390 2 153.7 10 1.9 94.5 21.2 FangOJ et al., 1996; Li YR et aI., 1990 lSI 427 3 215.7 25.1 4 79.3 -12 MengZF, 19901 0481 1 4.0 45.7 15.4 227.1 18.4 LI YA et aI., 1995 E 520 I 44.7 -46.7 9.8 2UX.2 -6 J LI YA et aI., 1995 K2) Alxablock (AL) (central reterence pomt:105.9°E, 37.2°N)

"2 I 355.2 50.3 5.7 327.5 8.6 HuangBC et al., 20001 C 3 2.9 23.6 11.1 296.4 4.5 He ZX et aI., 1988;HuangBCet aI.,2000 02-3 2 343.3 30.7 9.2 313.5 -3.5 He ZX et al., 1988;HuangBe et al., 2000 S 2 289.1 38.3 13.2 357.4 14.4 He ZX et aI., 1988;HuangBC et aI.,2000 0 3 187.5 20.2 11.3 111.1 5.7 He ZX et aI., 1988;HuangBCet aI.,2000 !Ol 1 38.6 48 144 219.5 14 He ZX et aI., 1988,Polarre-correctlOlj P) Qaidamblock(QD) (central reference point 96GE, 37.5°N) N, 1 189.4 72.9 11.8 20.9 34.6 Ge XH et aI., 1990 J3 1 212 55.5 7.1 32.3 17.7 Ge XH et al., 1990 J1 2 1 215 47 4.5 37.4 10.5 Ge XH et al., 1990 CI I 246.7 54.3 3.4 16.7 5.2 Ge XH et aI., 1990 PI 2 43.2 57 11.6 2U6.6 14.4 Ge XH et aI., 1990 K4) WestKunlun block(Kudiblock)(KX) (central reference point 77°E,36.5°N) J1 , 2 77.2 27.1 15.3 179.8 26.4 LI YA et aI., 19981 11'1 165.9 41.7 24.5 54.8 24 LI YA et aI., 19981 "I 188 60.6 19.6 29.7 22.1 LIYAet aI., 19981 [;-0 344.3 -31 18.5 245.5 -19.8 Li YAet al., 1998;480-510 Mal 816Ma 18.4 -71.5 13.7 18.4 -25.5 Li YAet al., 19981

~. EastKunlun Block(KD) (central reference point 94.6°E,35.9°N)1 [(2 209.3 60 18.9 28.9 19.8 LmJL & Watts, 19901 J1 313.3 53.4 4.5 339 5.5 WuGJ et al., 19981 fi28 Appendices

Conti.nuedJ ~trata N pp(o) Ap(O) CX95 D(O) P(O) Source@ Ih 256.1 42.3 3.8 15.1 -9.2 WuGJ etal., 19981 IT2 266.2 38.5 11.7 6.8 -15.2 DongXB et aI., 1991 IT, 229.3 30.2 5.6 38.8 -11.4 DongXB et aI., 1991 fl 288.3 41.4 8.1 349.5 -11.7 DongXB et aI., 1991 C 223.9 13 10.7 54.2 21.6 LmJL & Watts, 19901 ID 17.5 64 13.8 208.5 26.6 LmJL & Watts, 19901

10.Qiangtang Block (QT) (central reference point:92'E, 33.8°N) 01 2 126.27 -76.6 2.05 51.44 32.1 QwnF et aI., 19971 I(recent latItude of sample, 35.69°) N2 1 309.7 79.3 2.9 352.8 25.1 Ye XH et aI., 19871 E 1 202.4 55.1 8.8 34.1 16.9 LmJL & Watts, 19901 ~2 3 328.5 67.4 10.6 340.1 19.7 ZhouYX et aI., 19841 h 2 333.3 57.1 7.7 330.5 14.5 DongXB et aI., 1991 rI 2- 3 3 232.9 41.1 15.6 28.6 6.9 LmJL & Watts, 1990;LI YA et aI., 19951 fl 3 318.5 27.1 5.6 318.1 14.8 Ye XH et aI., 1987;DongXBet aI., 1991 K::l 5 312.5 22.5 13.4 319.8 -21.8 YeXH et aI., 19871 D2 1 328.7 7.3 9.4 296.2 -22.4 YeXH et aI., 19871

11.Gandise Block (GD) (central reference point:91.2°E,29.7°N)1 lEI 1 299.4 71.8 11 351.3 13.4 Allegreet aI., 1984 ~2 10 321.3 64.3 7.5 340 11.8 YeXH et al., 1987;Lin JL & Watts, 1990j ZhouYX et aI., 1984;Achache, 1989; Dongl IXB et aI., 1991; Zhu ZW, 198~ ~I 1 17.9 -10.5 13.6 252 8.9 DongXB et aI., 1991 1] 5 295.3 45.4 13.6 343 11.8 YeXHetal.,1987;DongXBeta1.1991;Zhul ZW et al., 198:'1 11 3 1 211.6 8.2 6 66.5 21.4 DongXB et aI., 1991 fl 1 271.2 36.8 9.7 359 23.5 DongXB et aI., 1991 K::J 1 288.7 41.1 6.8 346.3 -17.4 DongXB et aI., 1991 r:1-2 2 282.8 33 13.4 349 -26.1 DongXB et aI., 1991 D2 1 290 35.5 4.2 343.5 -22.4 DongXB et aI., 1991 S 1 263 24.3 4 9.2 -35.4 DongXB et aI., 1991

12.Himalayan Block (HM) (central reference point:89SE, 28.7°N)1 Q2-J 14 170.96 78.42 13.49 30.5 QianF, 1990(recentlatitudeof sample,31.5°1 QI 14 114.87 84.56 356.47 27.2 QianF, 1990(recentlatitudeof sample,31.5°1 1N2-Q 1 161.5 85.5 9.9 4.9 30 Zhu ZWet aI., 1984 N, 1 208 82.7 8.8 7 25 ZhuZWet aI., 1984 E 1 334.5 42.6 11 318.1 3 Zhu ZWet aI., 1984 ~2 3 312.4 47.9 6.5 332.8 4.3 DongXB et aI., 1991;Lm JL & Watts, 19901 1] 2 329.4 5.8 12.6 290.9 -22.9 YeXH et aI., 1987;ZhuZW et al., 198~ J, 1 326.5 3 11.3 290 26.9 Ye XH et aI., 1987;ZhuZW et aI., 19851 [[1-2 1 308 22.7 6.3 320 -26.6 Zhu ZWet aI., 198~ C 2 321.4 0.8 16.5 291.4 -32.3 Zhu ZWet aI., 198~ ID 2 335.4 -18.8 12.4 263.6 -29.6 Zhu ZWet aI., 198j S 1 283.7 28.3 5.8 345.3 -31.4 ZhuZWet aI., 198j PI 1 289.1 26.3 16 339.3 -31.9 ZhuZWet aI., 198j ~ppendlX 6 PaleomagnetIc Dataof ChmeseContment and Its Adpcent Area 42~

Conti.nuedJ ~trata N pp(O) Ap(O) CX95 D(O) P(O) Source@ !Ot 334.8 -30.9 6 250 -34 ZhuZWet a!., 198~

13.Indian Plate(ID) (central reference point 79'E, 21'Nj 5 22.5Ma 1 114.5 78.5 2.3 353 11.5 KlootwlJk, Radhakriehnamurty, 1981 25 35 1 136 72.5 3.5 345.1 10.9 KlootwlJk, Radhakriehnamurty, 1981 35=45 1 132 67.5 12 342 6.7 KlootwlJk, Radhalmehnamurty, 1981 45-55 1 121.5 -57.5 9 158.7 3.9 Klootwijk, Radhakriehnamurty, 1981 60-65 4 286.1 34.1 16.6 334.4 -29.2 Klootwijk, Radhakriehnamurty, 1981 IK2 100 66 17 294.7 21.4 5 318 -35.1 Klootwljk, Radhakriehnamurty, 1981 [

14.Baoshan-Sibumasu Plate(BS) (central reference point 99.1°E, 25.2°N)1 Jz 5 168.2 15.7 5 83.7 25.2 Liang,1990;ZhuangZH, 19951 11 3 2 174.5 -12 11.7 107.2 7.7 ZhuangZB, 1995 11'2 1 167.6 -2.4 15.1 101.8 18.3 ZhuangZB, 1995 K:3 6 317 33.4 13.6 326.6 -21.2 LiangQZ, 1990;ZhuangZH, 199~ K:I 1 296.3 33.1 12.7 343.5 -29.4 ZhuangZH, 1995 03 1 357.3 -57.5 11.1 216.3 -27.3 ZhuangZH, 1995 DI 5 356.3 -55.8 8.6 218.2 -27.7 LIangQZ, 1990; ZhuangZB, 199:) IS3 1 0.8 -68.3 9 204.1 -26.4 ZhuangZH, 1995 lSI 1 242 31.5 34 -23.1 LiangQZ, 19901 P3 5 2.6 -46.1 12 228.1 -22.2 LiangQZ, 1990; ZhuangZH, 199~ PI 5 2.6 36.7 20 237.8 19.7 LIangQZ, 1990;ZhuangZB, 199:)

15.Lanping-Simao-Indochina Plate(LI) (central reference point 101.4°E, 22.5°Nj E 1 70.8 85.5 9.6 358 30.5 LiangQZ, 19901 ~2 2 171.1 40 7.9 56 29.4 LIangQZ, 19901 ~I 3 171.9 37.1 10.4 59 28.8 LiangQZ, 19901 Jz 1 170.1 4.9 10.4 94 20.5 LIangQZ, 19901 11'3 3 171.5 5 21.8 103 16.2 LIangQZ, 19901 K:3 1 216.9 31.6 10 50.9 -7.9 LiangQZ, 19901 IS2 2 347.7 30.3 15.8 307.1 -7.3 LiangQZ, 19901 !'lakhonPlateau(IC) (central reference pomt 102.5'E, 16SN) 11-OMa 1 17l 86 5 4 17.9 Vandec Voo, 1993; Yang & Besse, 1993 K 1 176 79 8 11.2 19.3 Vandec Voo, 1993; Yang & Besse, 1993 1] 1 177 60 14 31.3 22.8 VandecVoo, 1993; Yang & Besse, 1993 fi30 Appendices

Conti.nuedJ ~trata N pp(o) Ap(O) CX95 D(O) P(O) Source@ Jz 178.5 62.1 7.7 29.1 21.1 Van der Voo, 1993;Yang & Besse, 1993 [f3-JI 181.6 57.4 5 34.2 19.7 Vander Voo, 1993; Yang & Besse, 1993 IT3 180 53 9 38.6 20.6 Vander Voo, 1993; Yang & Besse, 1993 IfI 172 49 8 43 25.8 Van der Voo, 1993; Yang & Besse, 1993 f2 356.2 58.4 6 213 22.5 Yang & Besse,1993 IP2- TI 332 -57 10.7 207.2 -22.9 Haile, 1981 (101.5°10, 3°N)1 C2-PI 344 55 11.2 212.3 17.8 HaIle, 1981 (lOISE, 3°N)1 CI 2 57 9.2 212.1 7.6 HaIle, 1981 (lOISE, 3°N)1 0 256 46 6.3 156.5 41.6 HaIle, 1981 OOISE, 3°N)1

16.Australia Plate(AU) (central reference point 135° 10, 25°S~

101 37 66 Ma 301 61 10 11.2 52.7 Van der Voo, 1993 K267 96 318 56 356.7 -58.9 Vander Voo, 1993 KI98-144 338 41 17 315.6 65.1 Van der Voo, 1993 Ih145-176 349 48 13 319.6 54.8 Vander Voo, 1993 1)1177-195 357 48 5 316 49.9 Van der Voo, 1993 T3216 232 350 32 291 -58.6 Vander Voo, 1993

T123) 245 342 42 314.1 -62 Vander Voo, 1993 P2246-266 320 43 348.4 -71.5 Van der Voo, 1993 PI 267 281 302 46 23.1 -66.6 Van der Voo, 1993

C2282 308 322 62 354.6 -52.7 Van der Voo, 1993

C1 309 365 141 84 0.7 -19 Van der Voo, 1993 ID3366 - 378 203 62 16 26.5 -12.3 Van der Voo, 1993 ID2379- 397 80 77 348.9 -17.1 Vander Voo, 1993 S2415-429 318 53.9 14.4 181.8 11.1 Van der Voo, 1993 0 1468- 505 20.6 -17 17 243.6 -13.6 Van der Voo, 1993 f; 506-543 20.3 -18 16 242.6 -13.3 Vander Voo, 1993

17.Southwest Japau (JP) (central reference point 133°10, 35°N)1

NI 5 222.5 73.6 11.9 19.8 33.5 Sasa]1ma, 1981 1101 7 216.4 56.7 6.7 40.1 32.1 Sasajlma, 1981 ~2 8 207.5 46 8.6 54.2 34.4 Sasajima, 1981 ~I 5 195 47.5 12.9 54.7 43.1 Sasajima, 1981 h 1 17 49.6 20 323.5 11.8 Sasa]1ma, 1981 11 3 2 347.2 58.8 13.5 342.9 8 Sasajlma, 1981 PI-2 1 295.4 55.6 7.4 9.8 1.8 Sasa]1ma, 1981 K:3 1 202.9 -21.3 8 118.8 3.1 Sasajima, 1981

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~u HN, Zhu RX, Bai LX et al (1998)Revisedapparent polar wanderpath of the Yangtze Block and its tectonicimplica] nons SCIence in Chma D 41(2): 182 1941 IWu HN, Zhu RX, Bar LX et aI (1999) Paleomagnellc results of PaleozOIc and MesozOIc rocks from Xmgshan-ZlgUlI sectIOn m HubelProvmce,South Chma.SCIence m ChmaD 42(2): 144=154J IYang ZY,Besse J (1993)Paleomagnetic study of Permianand Mesozoicsedimentaryrocksfrom NorthThailandsupportsl the extrusionmodelfor Indochma. Earthand PlanetarySCience Letters 117(3=4):525 55~ [Yang ZY,Ma XH, Sun ZM et al (1996) Preliminaryresult of Early Paleozoicpaleomagnetism in NorthernHenan and it~ significance. ChineseScienceBulletin42(4): 401-406. IYang ZY, Otofujl Y, Sun ZM et al (1998) Geomagnetic pole senes of boundary between Cambnan and OrdovIcIan lij langshan, Hebel.Chmese SCience Bulletm43(17): 1881-1885. lYe XH, LI JF (1987) PaleomagnetIsm and evolutIOn of Irbet plates and lethys Journal of ChengduCoIIegeof Geologyl 114(1): 65-79 (in Chinesewith English abstract). ghar Yongjlan, Zhou YaoxlU (1989) Paleomagnetism and tectomcevolutlonof North and South Chma Blocks smce th~ PhanerozOIc. Acta GeophyslcaSlmca 32(3):292-307 (m Chmesewith Enghsh abstract).1 ghang SH, Yang HX (1996)PaleomagnetIsm of the Jlamuslterranem the lateJurassIcepochand cretaceouspenod and It§ tectomc slgmficance, NE Chma Journal of Changchun Omverslty of Earth SCIences 26(2): 206-210 (m Chmese wlthl Englishabstract). Zhang SH, Zhu H, Meng XH (2001) New results of paleomagnetism of Devonian-Carboniferous in Yangtze block and their paleogeographical implications.Acta GeologicaSinica75(3): 303-313 (in ChinesewithEnglish abstract). ghao XX, Coe RS (1987) Paleomagnetlc constramtson the colhslOn and rotatIOn of Northand South Chma. Nature327: ~ ghao XX, Coe RS, Thou YX et al (1990) New paleomagnetIc results from northern Chma: colhslOn and sutunng wlthl Siberiaand Kazakhstan. Tectonophysics 181(1-4): 43-811 ~hao XX, Coe RS, GIlder SA et al (1996) Paleomagnellc constramts on the paleogeography of Chma: ImphcatlOns fori Gondwanaland. Austra.J. Earth Sci. 43(6): 643-672J Zheng Z, Kono M et al (1991) The apparent polar wander path for the North China block since the Jurassic. Geophys. Jour.Int. 104(1):29=401 ghou YX, Lu LZ, Yuan XG et aI (1984) Donnees paleomagnellques nouveIIes au Irbet-connarssance fundamental pourl Ie mouvementdu bloc de Lhasa. In: HImalayan Geology, II. pp.279 297. Geological Pubhshmg House, Beljmg (Iij Chinesewith Englishabstract). Zhou YX, Lu LZ, Zhang BM (1988)Preliminarypaleomagnetic researchfor Panxiregion.In: Zhang YX, YuanXC (eds) Contributionto Panzhihua-Xichang Rift, China. No.3. pp.212-230. GeologicalPublishingHouse,Beijing (in Chinese' with Englishabstract). ghu H, Zheng ZC, He XY (1987) Paleozoic Biostratigraphy and TectonicEvolutionof the Aha Massif Margin 159pp. Wuhan CoIIegeof GeologyPress, Wuhan(m ChmesewithEnghsh abstract)J ghu RX, Ischu KK (2001) Studies on Paleomagnellsm and ReversaIs of GeomagnellcfreId m Chma. 168pp. SClenc~ Press, Beijing. Zhu ZW,Teng JW (1984) Paleomagnetic proof of Indian Plate's dispersal toward north after the splitting of Gondwana' continentand its collision with Eurasia Plate. In: Productsof Cooperative Inspectionof HimalayabetweenChina and France, pp.17-23. GeologicalPublishingHouse,Beijing(in Chinese). ghu ZW (1985)Comparative significance of apparentpolar wanderpath of Xizangand its adjacentregionsfromPhanero­ ZOIC. Acta GeophyslcaSmlca 28(suppI.): 219-225. ghu ZW, Hao I Y, Zhao HS (1988) PaleomagnetIsm and Its ImphcatlOn of Pan-XI regIOn m MesozOIC. In: Zhang YXJ YuanXC (eds) Collectionof Pan-XiRift, China, (3): 199-211. GeologicalPublishingHouse,Beijing(in Chinese withl Englishabstract). Zhuang ZH, Tian OX, Ma XH et al (1988) A paleomagnetic study along the Ya'an-Tianquan Cretaceous-Eogene section! in Sichuanbasin.Geophysical & GeochemicalExploration12(3):224-228 (in Chinesewith Englishabstracu] ghuang ZH (1995) Research on plaeomagnetism of Hengduan Mountains and its adjacent areas. Chengdu Institute ofj GeologlcaI MmeralProducts,Mmlstryof Geologyand MmeraIResources(m Chmese)J ~.. ~ppendix17Temperijture, Pres$ure, DeptJll and Tbeljmal Gradient in Rock Forming Stages of Chinese Continent

!The calculating method of thermal gradient in crust Ishowed in C~apter13.In ~etable, M ib the depth 0tMohorovfcfc discontinuity, according ~oth, ~eterrnined4ta, C is the depth of crust,IL is the depth of lithosphere bottom FTiFission Track method; TL Thermoluminescence technique.

Forming Thermal Isotopic Temperature Press4 re Are Rock depth gradient Sources age ($a) ('1(::) (GP~) (krn) ("CIkrn)

Early Mesoproterozoic Changcheng Period 1,800-1,4001\.1a Laixi-Laiyang Granulite 1,752 860 >1.4 46.7 21 Liu et al., 1998 Shandong

West Miyun, Beijing ranet 774 0.957 31.9 24.2 Chen et al., 1914 > 1'~17 East Miyun, Beijing nelusion > 1,717 856 1.23 41 22.7 Chen et al., 19 4 South Jilin ~reen schist ~I, 0 660 0.8 26.7 25 Cheng et aI., I 94

Late Mesoproterozoic Jixia Period 1,40f)j-1,000 Ma Mudanjiang, ~eilongjiang mphibolite 370 0.7 23.3 15.9 Cheng et al., Ij94 Kuanping Gro p, Qinling reen schist 550-~500·4--016 13-20 13-30 Liu et al., 1993 Kuanping Gro p. Qinling reen schist 650 0.6 20 33 Zhang et aI., I 91 Kuanping Gro p, Qinling reen schist 550 0.5 16.7 33 Cheng et aI., I 94 Hong'an Groll. Dabie reen schist 600 0.63 21 28.6 Hubei Geologi al Survey, 199 Wudang Grou reen schist 350 0.6 20 17.5 Liu et al., 1993 WudangGrou ylonite 300 0.2 10 30 Liu et al., 1993 Xilingol, Inn~MongOlia mphibolite 550 0.6 20 27.5 Zhao et aI., 2~2 South Dulan, inghai clogite 900 913 >2.0 66.7 34 Yang et al., 2 0 Sibao Group, iangnan reen schist 3 250 0.2 6.7 37 Cheng et al., 1 94 Songshugou, inling ranulite ~ I, 0±46 800-~001.3- 116 43-53 18-20.6 Zhang et aI., 2 01 Yanggao, Sha i imberlite 1,183 (?) 1200 2.5-35 82-115 10.4-15 Chi et al., 199( Tieling, Liao ng imberlite 701- ,181 150L Chi et al., 199(

Early Neoproterozoic Qing 'aikou Period 1,000-800 Ma

IOgite 1.27 42 18 Liu et al., 1993 Hongan Gr0i' Dabie 1,00Of-800 683 Qinling Grou , Qinling uphibolite 990-~00 720 0.9 30 24 Liu et al., 1993 Songshugou, inling roxenolite 983 828-~87 1.4-116 50 21 Liu et al., 1994 Songshugou, inling ranulite 983 765-~25 1.03 34.3 24 Liu et al., 1994 Songshugou, inling nphibolite 983 ~62 ~0.9 30 19-28 Zhang, 2001 Hongan Grou , Dabie ~een schist ~80 500 0.55 22 23 Liu et al., 1993 i0. is' .a Cont filled :ij £i Forming Thermal e Isotopic Temperature Pressure >< depth gradient Area Rock age (Ma) (''C) (GPa) Sources (km) (''CIkm) ~I Jiaonan Group, Shandong Eclogite ~800 650 1.6 53.3 13.3 Su et aI., 1994 .§ Su-Lu collision zone Eclogite 900-720 1,100 3.1 103 12 Zhang et aI., 2002 Yukahe, North Qaidam Eclogite 950-850 >732 2.8 80 9.2 Liet aI., 1999 ~800 i Dikou formation, Fujian Anphibolite 625 0.4 13.3 47 Fujian Geological Survey, 198 Yunkaidashan, Guangdong Granulite 950 650 0.52 17.5 54 Zhou et aI., 1997 ~I Yunkaidashan Granulite 813--638 883 0.71 23.7 37 Du et aI., 1999 Yuanmou, Yunnan Anphibolite 1,000-820 630 0.8 26.7 23.6 Deng et aI., 2001 ~~ North Qaidam Eclogite NP 722 2.2 73.3 9.8 Yang et aI., 1998 Beishan, Gansu Eclogite NP 800 > 1.6 53.3 17.6 Mei et aI.. 1998 Bixiling, Dabieshan Eclogite NP 775 4.76 159 4.9 Liu et aI., 1995 Border among Shaanxi, Gansu and Sichuan Glaucophane 1,000-800 400 0.6 20 20 Wei et aI., 1994 Green schist 1,000-800 400 0.4 13.3 30 South Dabieshan Migmatization 848 580 1.4 46.7 12.4 Wei et aI., 1997 East of East Kunlun Gneiss NP 820 I 33 24.8 Chen et aI., 1999 Gangbian, Jiangxi Monzonite ~847 750 I 30 25 Li et aI., 1997 Gangbian, Jiangxi Basalt ~847 1,000 0.7 55 23 Li et aI., 1997 Lushan, Jiangxi Granite 823 565 0.57 19 24 Li et aI., 1998

Late Neoproterozoic-Early Cambrian Period (Nanhua-Sinian-Early Cambrian) 800-513 Ma Rizhao, Shandong Eclogite 613.3 981 2.95 98.3 10 Zhang et aI., 1999 Jiaonan, Shandong Green schist >574 458 0.73 24.3 18.8 Su et aI., 1994 Middle Altun Metam. shale >570 550 2 66.7 8.2 Liu et aI., 1999 South Altun Eclogite > 519 830 1.85 61.7 16 Liu et aI., 1999 Altun Mylonite 574.68 550 2 66.7 8.2 Che et aI., 1995 East Dabieshan Gneiss 772 515 0.75 25 20.6 Dong et aI., 2002 Kudi, Southwest Xinjiang Anphibolite Sinian 993 1.66 55.3 22.6 Sheng et aI., 1996 Kudi, Southwest Xinjiang Peridotite Sinian 993.2 2.39 62.3 20.6 Sheng et aI., 1996 Ulausu, Inner Mongolia Anphibolite 638--607 670 0.3 II 61 Zhang et aI., 1996 Ondors Inner Mongolia Basalt 624 400 0.7 23.3 17 Zhang et aI., 1998

Early Paleozoic Qilianian Period 513-397 Ma Ondor Sum Group, Inner Mongolia Green schist ~400 450 0.8 26.7 19 Inner Mongolia Geological. S rvey, 1991 Harkshan, Xinjiang Anphibolite 456-415 425 0.8 26.7 16 Cheng et aI., 1994 Xitieshan, Qinghai Eclogite E. Paleozoic 830 >1.4 46.7 20.4 Zhang et aI., 2002 DaQaidam Eclogite E. Paleozoic 730 2.8 93 8 Zhang et aI., 2002 Continued Forming Thermal Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (km) ("CIkm) Qinling Group nphibolite 425 760 0.6 20 38 Liu et al., 199 North Qinling nphibolite 450- 80 767 0.7 23 31 Zhang et al., 2$01 North of East~inling asalt 403.5 1190 1.36 45.3 31 Wang et al., 1<191 Maoji, Tongb shan nphibolite 575 34 600 0.7 23.3 26 Liu et al., 199 Maoji, Tongba shan een schist 467 11 520 0.6 20 26 Liu et al., 199 North Qilian nphibolite ~4 550 0.8 26.7 20.6 Cheng et al., 1994 North Qilian laucophane 46 150-~500.4-017 13-23 11 Wu et aU 993 North Qilian laucophane 46 > 38 0.6-07 20-23 16-19 Wu et al.1993 North Qilian logite 46 340 0.8 26.7 13 Wu et aLl993 North Qilian hengite 455 40 350 0.75 25 12.5 Zhang et al., I~98 Middle of NO! Qilian arnet >46 400 0.65 21.7 18.4 Zhang et al., 1~98 North border Qaidan logite 465 850 2.5 83 10.2 Lai et al., 199( North border Qaidan nphibolite 465 520 0.52 17.3 30 Lai et al., 199( North border Qaidan logite 466 730 2.8 93 8 Yang et al., 1918 WestAltun logite 8.6 Zhang et al., I 99 503~00860 3 100 WestAltun ranulite 447 62 850 1.2 40 21.3 Zhang et al., 1 99 WestAltun logite 503- 00 850 3 100 8.5 Zhang et al., 2 02 Altun 'eridotite 494.6 970 5.1 > 100 9.7 Liu et al., 200 WestAltun 519 500 0.5 18.5 27 Liu et al., 199(

~~~~~~:: South Tianshai ' 440 964 1.42 47.3 24 Wang et al., 1<199 South TianshaJ ranulite 813 1.5 50 19 Su et al., 1996 South Tianshai laucophane 452i2450- 50 375 0.65 21.7 17.3 Gao et al., 199, Jianglang,Wes Sichuan phibolite 525 555 0.38 13 43 Yan et al., 199 Yunlu,West G angdong ranulite E. Pal ozoic 836 0.69 23 36 Chen et al., 1994 Jianyang-Ch gping nphibolite ~4()( 650 0.28 9.3 70 Fujian Geological Chong' an-Shi heng ~phibolite ~4()( 575 0.3 10 57.5 Survey, 1985 Kalpin, Xinjia g andstone-shale Cam 'an 24-22 Wei,1989 Kalpin, Xinji g andstone-shale Ordo ician 22-21 Wei,1989 Erdos basin andstone-shale E.Pal ozoic 25-30 Ren,1996

Mengying, Sh mberlie t 457± 1,184 6.75 222.7 L 5.3 Chi et al., 199 Fuxian, Liaoni imberlite 462.7 4.8 1,123 6.3 208 L 5.4 Chi et al., 199 Yingxian, Sh: xi imberlite E. Pal ozic 1,113 5.2 172L 6.5 Chi et al., 199 Langao, Sha i ~roxenite 431.9 1,350 3 100L 20 Huang, 1993 North Qilian 'eridotite 495- 22 1,093 4.28 132L 8.3 Song and Su, 1998 NorthQilian 'eridotite 495- 22 1,100 4.2 140L 8 Su et al., 1999 {I Xiawan, Zhejiang dmellite E. Pal ozic 20 Yang et al., 19 6 is ~ ~ Con Inned £i &. Forming Thermal x Isotopic Temperature Pressure depth gradient -..J Area Rock age (Ma) (OC) (GPa) Sources (Ian) ("CIkm) (;l .g Zhuzhou, Fujian Admellite E. Paleozic 21.5 Yang et al., 19 6 Ninghua, Fujian Admellite E. Paleozic 29.5 Yang et al., 19 6 East Qinling-Tongbai Tholeiite 403.5 1,190 1.36 45 31 Wang et al., 19 I ,I

Late Paleozoic Tianshanian Period 397-260 Ma ~ Altay, Xinjiang Basalt M. Devonian 1,300 0.5 18.5 70.3 Niu et al., 199 West Junggar Lherzolite L. Paleozoic 1,100 1.6 53.3 26 Zhao et al., 19 3 ~~ u West Tianshan Eclogite Devonian 530 1.9 63.3 8.4 Zhang et al., 2 fao .g South Tianshan Pyroxenite 315 964 1.4 47.3 24 Wang et al., 19 9 9­ South Tianshan Glaucoph. 345 375 0.65 21.7 17.3 Gao et al., 199 § Longmenshan, Sichuan Anphibolite E. Permian 500 0.5 16.7 30 Sichuan Geolo 0- Jinshajiang, Sichuan Anphibolite E. Permian 600 0.48 16 37 Survey, 1991 ;l Lancangjiang Anphibolite Permian 735 0.5 16.7 44 Zhong, 1998 ~ West Tianshan Eclogite Devonian 530 1.6-1.9 53-63 10 Zhang et al., 2 faO ~ West Junggar Granulite > 320 1,100 I 33 33 Zhang et al., I 98 Fuping, South Qinling Anphibolite 285-240 688-693 0.6 20 34 Zhang et al., I 98 ~ Fuping, South Qinling Anphibolite 260 570-598 0.7-1 23-33.3 18-26 Zhang et al., I 98 g North China Sandstone-shale Carbon.- reflectivity 25~30 Ren et al., 200 5' Permian Tarim basin Sandstone-shale Carbon.- of coal 32~29 Pan et al., 199( ,.,.~ Permian Shiwandashan Sandstone-shale Carbon.- 40~50 Wang, 1998 ~ Permian 5' NW Jnnggar Sandstone-shale Permian reflectivity 20~25 Zhang et al. 19 9 (jq en Tarim basin Sandstone-shale Carbon.- of coal 30 Fan et al., 199( Permian ~ Erdos basin Sandstone-shale Carbon.- 22~24 Ren, 1996 g., Permian ne- Zhenyuan, Hunan Garnet ~360 1,250 5.2 172L 7.3 Lu et al., 1997 5' Yuanshui, Hunan Daimond ~ 360 (?) 1,350 5.8 192L 7 Lu et al., 1997 cc nc Dahongshan, Hubei Peridotite 326-352 1,150 3.39 120L 9.6 Liu et al., 1991 g Minggang, Qinling Peridotite Carboni. 870 1.3 43 22.6 Lu et aI., 1997 5' Wuyueshan, Dabieshan Granitoid 376 0.56 18.6 Ma et al., 1995 g Muojiang, Yunnan Pyroxene- Carboni. 1,212

Indosinian Period 260-200 Ma Dabieshan Eclogite 243-221 750 I 33 ~23 Chen et aI., 19 4 Dabieshan Eclogite 243-221 1,000 4 133 7.5 Chen et al., 19 4 Dabieshan Eclogite 243-221 896 2.05 68 16 You et aI., 199 Luotian, Dabieshan Migmatite Triassic 800 0.5 16.7 48 You et al., 199 Shuanghe, Dabieshan Jadeite-quartz Triassic 800 1.31 43.6 20.4 Han et aI., 199 Shima, Dabieshan Eclogite 243 850 2.8 93 9 Xiao et aI., 19\ 3 Shima, Dabieshan Eclogite 217 650 1.4 47 14 Xiao et al., 19\ 3 East Dabieshan Anphibolite 243-221 850 2.8 93 9 Xiao et aI., 19\ 3 Dawu, Dabieshan Eclogite 243-221 500 1.6 53 9.4 Ma et aI., 1995 Bixiling, Dabieshan Eclogite 250--230 700 2.7 90 7.8 Zhang et al., I 95 Dabieshan Clinohumite 250--230 800 6.7 223 3.5 Zhang et al., I 95 Hong' an, Dabieshan Glaucophane 243-221 500 0.7 23 22 Liu et aI., 1993 Dabieshan-Sulu Marble Triassic 660 3.5 116.7 5.7 Cong et aI., 19 9 South Dabieshan Zoisite 220--210 600 l.l 36.7 16.3 Jiang et al., 19 9 Tongbaishan Eclogite 250--210 780 1.4 47 19 Suo et al., 2001 Dabieshan Collision Eclogite Triassic 800 > 2.8 > 93.3 8.6 Zhong et aI., 2 01 Fuping, Qinling Granulite 220 720--770 0.6 20 36-38.5 Zhang et al., I 98 Rongcheng Eclogite 232 797 1.8 60 15.6 Ye et aI., 1992 Dabieshan, Anhui Daimond inclu. Triassic > 900 >4.0 > 133 L 6.8 Xu et aI., 1991 Huashanzhai, Hubei Alkali rock 215 1,120 0.7 23.3 48 Li et al., 1991 Xinxian, Henan Eclogite 240--210 650 3 100 6.5 Zhang et al., I 93 Dabieshan, Anhui Eclogite 250--210 > 600 > 2.5 83.3 7.2 Du et aI., 1998 East Dabieshan Mica schist Triassic 630 2.4 80 7.9 Jiang et al., 19 8 Dahingganling-Yanshan Granulite 229 900 I 33.3 27 Shao et al., 20<2 Ninghua,West Fujian coal metamorph. E. Triassic 923 33M 28 Yang et al., 19 6 Datian, Middle Fujian coal metamorph. E. Triassic 849 37M 22.9 Yang et al., 19 6 Nan'an, East Fujian coal metamorph. E. Triassic 887 43M 23 Yang et al., 19 6 Qiangtang, Xizang Glaucophane 222.5 420 0.72 24 17.5 Li,1997 Shuanghu, NorthXizang Glaucophane 222.5 460 0.75 25 18.4 Bao et al., 199 Santanghu Basin Sandstone-shale Triassic 35 Zhou et al., 19 8 Youjiang Basin Sandstone-shale Triassic reflectivity 40-43 Suo et aI., 199 Shiwandashan,Guangxi Sandstone-shale E.-M. Trias. of coal 40-45 Wang et al. 19 8 Jinhua, Zhejiang Granitoid Triassic 28 Yang et al., 19 6 i0. is' .a ~ Con Inned £i &. Forming Thermal x Isotopic Temperature Pressure depth gradient -..J Area Rock age (Ma) (OC) (GPa) Sources (Ian) ("CIkm) (;l .g Shaoxing, Zhejiang Granitoid Triassic reflectivity IS Yang et al., 19 6 West Fujian Granitoid Triassic of coal 60 Yang et al., 19 6 East Fujian Granitoid Triassic 22 Yang et al., 19 6 ,I Rongcheng, Shandong Peridotite 232 1,033 5.27 175L 6 Ye et aI., 1992 Horqin, Inner Mongolia Granulite Triassic 900 1 33.3 27 Han et al., 200 ~

Yanshanian Period 200-135 Ma ~~ u Bixiling, Dabieshan Anphibolite 179 450 0.7 23 19.6 Suo, 2001 .g North Dabieshan Gneiss 151-133 700 0.76 25.3 27.7 Sun et al., 199 9­ Dabieshan Anphibolite 180-140 560 0.7 23.3 24 Zhao et al., 19 9 § East Dabieshan Metam. granite 190 650 1 33.3 19.5 Xu et al., 1998 0- Luotian Dabieshan Granulite Jurassic 900 1.1 > 30 30 Jin,1997 ;l Dabieshan 600 0.6 20 30 Zhong et al. 19D8 200-170 ~ Xiaoqinling Epidote 160-135 498 1.03 34.2 14.6 Liu et al., 1998 ~ Xiaoqinling Epidote 160-135 652 0.476 15.9 41 Liu et al., 1998 Lancangjiang Glaucophane 193 390 0.67 22.3 17.5 Zhang et al. 1990 ~ Pingdang-Dongshan Mica Schist 202-166 717 0.62 20.7 34.6 Chen et al., 19 7 g Ninghua, Fujian Coal metam. M. Jurassic 905 32 28.3 Yang et al., 19 6 5' Datian, Fujian Coalmetam. M. Jurassic 809 31 26.1 Yang et al., 19 6 Nan'an, Fujian Coal metarn. M. Jurassic 863 34.3 25.2 Yang et al., 19 6 ,.,.~ North Hubei Glaucophane 185.1 450 0.7 23.3 19.3 Niu et aI., 199 East Guangdong Green schist L. Jurassic 600 0.7 23.3 25.8 Chen et al., 19 4 ~ Changle-Nan'ao Green schist 178-165 800 0.86 28.7 27.9 Chen et al., 19 4 5' Daqing oilfield Coal metarn. L. Jurassic Wu et al., 1991 (jq 33 en Santanghu basin Sandstone-shale Jurassic Reflectivity of coal 27-28 Zhou et al, 199~ Jiuquan basin Sandstone-shale Jurassic 37.5-45 Ren et al., 200 ~ Xinshuai basin Sandstone-shale Jurassic 47.3-61 Ren et al., 199 g., Reflectivity of coal Junggar basin Sandstone-shale Jurassic 30-20 Zhou et al., 19 9 ne- Erenhot basin Sandstone-shale Jurassic 35-55 Ren et al., 200 5' Reflectivity of coal cc Erdos basin Sandstone-shale Jurassic 36-41 Ren et al., 199 n Turpan-Harni basin Sandstone-shale Jurassic ~30 Ren et al., 200 c Reflectivity of coal g Tarim basin Sandstone-shale Jurassic ~25 Ren et al., 200 5' Tarim basin Sandstone-shale Jurassic 26-29 Pan et al., 199t g Shiwandashan Sandstone-shale E.-M. Jurassic 20-30 Wang, 1998 Daqing oilfield, Heilongjiang Granite in Jurassic Reflectivity of coal C Compiling Gr up of Petrale. Geo. NEand S-N 1993 t; '.Q Continued !

Forming Thermal Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (km) ("CIkm) Daqing oil field, Heilongjiang facite m NJ' NNE M.-L1Ufassic C Compiling GrIUPof Geo. 1993 .; Daqing oil field, Heilongjiang j;:~~tem N , NNE Earli st Cret. C Compiling Gr up of Petrole Geo. rend 1993 Mingyuegou asin, Yanbian, t·lin ::tyroxemtemel sian M. Jurassic 991-1,158 0.55-0.96 32-37 ~30 Wang et al., 2 5 Yanbian, Jilin roxenite mel SIan M. Jurassic 25-37 Zhao et 31., 20 5 Baishishan, Z angguangcailin , Jilin ranitoid 196 C-M Sun et al., 200 Dahingganling anitoid Jurasf·c C-M Lin et 31.,2(){)L Northern Dahi gganling Ikalic volcanid rock L. Jur sic C-M Yin et al., 200, Jiulianzhuang, Dahingganling yenite 137.5 C-M Xue et al., 200 Hatumo River, Dahingganling acite 154- 47.3 C-M Xue et 31.,200 Baiyinnu ore eld, Dahingganling gnimbrite 160.3 C-M Xue et 31., 200 Manituxi Mou t, Dahingganling acite 149 C-M Xue et 31., 200 Wudan, Middl Dahingganlin] uff 152.3 C-M Xue et 31.,200 Du'erki, middl Dahingganlin ranitoid in NE1trend E. Jurassic C-M Xiao et al., 20c/4 Ma'anzi, sou ern Dahingga~nng ranitoid in NE trend L. Jurassic C-M Xiao et al., 20C/4 Huangganglia g, southern D ingganling lagio granite 142 C-M Xue et 31., 200 Gedenghua, s them Dahingg nling dmellite 185 C-M Xue et 31., 200 Haisuba, south rn Dahingganl ng omblendite 202 C-M Xue et 31., 200 Baiyinnuo, eas ern Inner Mon alia ranodiorite In NE E. Jurassic C-M Xiao et 31.,20 rend Taibudai, easte Inner C-M Xiao et al., 20 Mongiia ranite in NE~endE. JUff-Sic Baishilazi, eas em Inner Mon alia ranitoid in N trend E. JUf sic C-M Xiao et 31.,20 Mogutu, easte Inner Mongo ia ranitoid in N trend E. Jur ssic C-M Xiao et a!., 20 Wulantao, east rn Inner Moog lia ranitoid in N trend E. Jur sic C-M Xiao et al., 20 Chabuganshan Tianshanxian yolite 164 C Chen et 31., 19 Lubeixian, Inn r Mongolia ndesite, igni rite 167.2 C Chen et al., 19 7 Duijiugou, Fe gzhen, Inner Mongolia inette and Ga bro 144-~46.6 L Shao et 31., 20 5a Uliji, 104°23.I'E, 40 054.8'N anodiorite 207.7jU-Pb C-M Hong et al., 20 3 East Baotou, I ner Mongolia honkinite 198± C-M Yan et 31.,200 Liangcheng, I ner Mongolia honkinite 190± C-M Yan et 31.,200 Well Kacan-I, Jianchang, Liaoning 'rachyandesite lmd tuff 146-~65.6 C-M Chen et al., 1997

Xinglonggou ormation, Liaoning citein ENE frend 199-~89 C Lu et 31.,2005 Wulong, easte Liaoning rarute 136 C Wei et 31., 200 Wulahada, we t Liaoning ~desite in NNp 142.4 C-M Zhang et 31.,2~0l Guancaishan, iaoning ndesite 134.6 C-M Zhang et 31.,2~0l i0. is· .a -;J> '0 Contmued (1) Forming Thennal "&. Isotopic Temperature Pressure x Area Rock depth gradient Sources -..J age (Ma) (OC) (GPa) (km) (OCIkm) (;l '0a Haifanggou, Beipiao, Liaoning Rhyolitic tuff 140 C-M Chen et al., 1997 (1) Lanqidouggou, Beipiao, Liaoning Andesite 141.6 C-M Chen et al., 1997 ~ Huaziyu Magnesite Mining, Liaoning Lamprophyre ISS L Jiang et al., 2005 @ Da' ertaizi, Songlingmen, Chaoyang Andesite 166 C-M Chen et al., 1997 Yanshan Granitoid 170-135 0( 900 0.9-1.7 30-56 30-16 Wang, 2002 '" C-M ~ Badaling, Beijing Granitoid Jurassic C Zhang, 2001 ~~ Chahe, Zhulu, Hebei Diabase 153.6 L Shao et aI., 2005a U Fengning, Hebei 125.2-157.4 Wu et aI., 1984 .g Granitoid C 9- Kuancheng, Hebei Granodiorite 162 C Wu et aI., 1984 cc Beichagoumen, Northern Hebei Diorite, quartz, syenite, 146.2-147.6 C Chen et al., 2004 0- "-3 granodiorite e- Tiaojishan Formation, Luanping, Hebei Andesite 162.8 C Zhang, 2006 (1) Zhangjiakou Formation, Luanping, Hebei Rhyolite 135.7-135.2 C Zhang, 2006 a~ Handan, Hebei Peridotite inclusion E. Jurassic 1,008 1.7 57.7 18 Xu et aI., 1991 o OJ Xiabancheng, north Hebei Trachyandesite in NE 171-186 C-M Li et aI., 2004 &. (1) Shexian, south Hebei Gabbro in NNE ISO C-M Hong et al., 2003 g Laiyuan, Hebei Gabbro in NNE 140 C-M Hong et al., 2003 5' South Taihang Mts. Peridotite inclusion ~ 170 1,000 2.7 90L 11 Xu et aI., 1993 ~ 0 South Taihang Mts. Mafic inclusion ~170 1,000 2.1 70L 14 Niu et aI., 1994 ,.,. Lingloug Shandoug Granitoid with foliation 166-153 750 0.45 20C 37.5 Wan et aI., 2001 " Linglong, Shandong Granitoid with foliation 155-160 C Luo et aI., 2002 ~ Luanjiahe, east Shandong Granitoid with foliation 155-160 C Luo et aI., 2002 5' Weudeng, east Shandong Admellite 159.8 C-M Guo et al., 2005 (jq en Dougushan, Shandong Granodiorite 160.7 C-M Guo et aI., 2005 0;' (jq Sanshandao, Jiaojia, Shandong Granite M. Jura. 11-15 Sun, 1994 ~ Western Shandong granodiorite 7.4-11 Sun, 1994 -.,0 Guojialing, Shandong Granodiorite in WNW 148-134 700 0.5-D.28 34C-M 21 Chen et al., 1993 ne- Gudao, Zhuangxi 5 area, Jiyang, Shandong Andesite, basalt Mesozoic C-M Compiling Group of Petrol. Geo., 5' cc 1993 n Birman, Gudao, Jiyang, Shandong Diorite porphyry Jurassic C-M 199~ 0 Compiling Group of Petrol. Geo., g Jiyang, Shandong Lamprophyre Jurassic C-M Compiling Group of Petrol. Geo., 199 5' (1) Ta'ershan, south Shanxi Monzonite-diorite Jurassic C-M Zeng et al., 1997 g Laoshan, south Shanxi Quartz syenite Jurassic C-M Zeng et al., 1997 Jiaojieshan, south Shanxi Aegirine-augite syenite Jurassic C-M Zeng et al., 1997 Wutaishan-Hengshan, Shanxi Granite-porphyry Jurassic C-M Zhen,2004 ~ Continued ! Forming Thermal Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (krn) ("CIkm)

Orite Pingshun-Hug an, south Shanxi i 154-~58 C-M Shanxi GeOlo;cal Survey, 19 9 Zhujiagou, Tia zhen, Shanxi iorite 140.4 C Shao et al., 20 5a Qixian, Middl Shanxi Ikali quartz syenite C Shanxi Geolo .cal Survey, 19 9 Zijinshan, Da shan, JiaOpais~an,Linxian ~lkali complex J:;;:liC C Shanxi Geolo .cal Survey, 19 9 Huyanshan, G jiao-Jiaocheng Shanxi yenite Juras ic C Shanxi Geolo .cal Survey, 19 9 Gudongdao-Xi aling, Jiaoch ng, Shanxi yenite Juras ic C Shanxi Geolo 'cal Survey, 19 9 Xixianding-Xi e, yenite Juras ic C Shanxi Geological Survey, 19 9 Gujiao-Jiaoch ng Dongxianding Shangbai- yenite Jurassic C Shanxi GeOIOjcal Survey, 1919 quan, Gujiao-J aocheng, Shanii Mulianpo-Ku gquan, yenite Jurassic C Shanxi Geolo 'cal Survey, 19 9 Gujiao-Jiaoch ng Longzhuangg , Heishany: Zhuanger- Quartz syenite porphyry Jurassic C Shanxi Geological Survey, 19 9 shang, Jiaoche g, Shanxi NW Huyansha , GUjiaO-Jiaocteng, Shanxi -j'\egirine-aUgitelsyenite Jurassic C Shanxi Geological Survey, 19&9 Longzhuangg -Ketoudongta un, .f\.egirine-augite Syenite Jurassic C Shanxi Geological. Survey, 1989 Gujiao-Jiaoch ng, Shanxi Longwangmia -Yichengxian, hanxi Quartz monzonlte Jurassic C Shanxi Geological Survey, 19&9 Laoshan-Qiao' rjiao- Quartz monzon te Jurassic C Shanxi Geological Survey, 1989 Yutuling, Xian fen Ta' ershan, Xi gfen- uartz_monzojte dior­ Jurassic C Shanxi Geological Survey, 1989 Quwo-Yichen Shanxi te Hanjiayan- He laoding, Xiangfen, Shanxi uartz-monzo ire dior­ Jurassic C Shanxi Geolo~calSurvey, 19~9 te Shengwangsh -Shanchahe-Jiaojie­ uartz-rnonzo .te dior­ Jurassic C Shanxi Geolog~calSurvey, 19J9 shan, Shanxi te Yanwowa, No west uartz-rnonzo .te dior- Jurassic C Shanxi Geological Survey, 1989 Yicheng, Shan i te

South Ta' ersh: , Shanxi onzonite JUraS~ic C Shanxi GeOlo~'cal Survey, 1919 Guniangshan, orthwest Yicheng, Shanxi ranite porphy Juras ic C Shanxi Geolo 'cal Survey, 19 9 Dagushan-Zi ashan, yenite Juras ic C Shanxi Geolog] cal Survey, 19 9 Fushan-Xiang n-Yicheng Longwangmia -Hanjia-Yan, Xiangfen, yenite Jurassic C Shanxi Geolo~calSurvey, 19~9 Shanxi Zhoujiazhuan -Cijiao- odium Syenite Jurassic C Shanxi GeoloJcal Survey, 19J9 cun, east Xian fen, Shanxi i0. is' .a Con inued ~ £i Forming Thermal &. Isoto ic Temp rature Press re x Are ock depth gradient Scurces -..J age (~a) (9 ) (GP) (km) ("CIkm) (;l East to Zhouji zhuang, egirine-augite Syenite Juras ic C Shanxi Geolog·cal Survey, 19 9 .g east Xiangfen, Shanxi South Ludings an, Quwo, Sha nxi ::!uartz Syenite iorite Jurassic C Shanxi Geolog'cal Survey, 19 9 ,I Qiaoshan, nort Quwo, ::!uartz Syenite iorite Jurassic C Shanxi Geolog·cal Survey, 19 9 Shanxi ~ Yangtancun, N orth Quwo, Sha nxi ::!uartz Syenite iorite Jurassic C Shanxi Geolog·cal Survey, 19 9 Heshangweng uishan, Yichen , Shanxi Juartzmonzoni te Jurassic C Shanxi Geolog·cal Survey, 19 9 ~~ Erfengshan, so uth Fushan, Sh nxi yenite diorite Jurassic C Shanxi Geolog'cal Survey, 19 9 u Sikongshan, scuth Fushan, Sh mxi vlonzonitc Jurassic Shanxi Geolog·cal Survey, 19 9 .g C 9­ Tiantanshan-S iliyuan, yenite diorite Jurassic C Shanxi Geolog·cal Survey, 19 9 § East Fushan, S anxi 0- Xincun-Beiye, Yicheng, Shan i yenite diorite Jurassic C Shanxi Geolog·cal Survey, 19 9 ;l Shitancun, NE Yicheng, Shan i yenite diorite Juras ic C Shanxi Geolog·cal Survey, 19 9 ~ Xincun-Beiye, Yicheng, Shan i yenite diorite Juras ic C Shanxi Geolog·cal Survey, 19 9 ~ Southeast Lin£ n, Shanxi '\egirine-augite Syenite Jurassic C Shanxi Geolog·cal Survey, 19 9 Hejiazhuang-S icunshan, sou heast Linfen, '\egirine-augite Syenite Jurassic C Shanxi Geolog·cal Survey, 19 9 ~ Shanxi g Guanquecun-Liangjiapo, e st Linfen, '\egirine-augite Syenite Jurassic C Shanxi Geolog·cal Survey, 19 9 5' Shanxi Qingyangling outheast Xiang en, Shanxi yenite diorite Jurassic C Shanxi Geolog'cal Survey, 19 9 ,.,.~ Songcun, east iangfen, Shan i yenite diorite Jurassic C Shanxi Geolog·cal Survey, 19 9 Dapocun, sout east yenite diorite Juras ic C Shanxi Geolog·cal Survey, 19 9 ~ Xiangfen, Sha ixi 5' Pandao,Xiang n, Shanxi )iorite porphyr Juras ic C Shanxi Geolog·cal Survey, 19 9 (jq en Dongzhangcun -Xiangfen, Sha xi yenite diorite Juras ic C Shanxi Geolog'cal Survey, 19 9 Xihaicun, east Quwo, Shanxi yenite diorite Jurassic C Shanxi Geolog'cal Survey, 19 9 ~ Ganjuncun, Yi heng, Shanxi yenite diorite Jurassic C Shanxi Geolog·cal Survey, 19 9 g., Pingshun-Ling huan, SE Shan i )iorite Jurassic C Shanxi Geolog·cal Survey, 19 9 ne- East Pingshun, SE Shanxi yenite diorite Jurassic C Shanxi Geolog·cal Survey, 19 9 5' O' Xingcheng-Pu huicun, )iorite Jurassic C n southeast Shan i c g Yetou-Zheshui un, yenite diorite Juras ic C Shanxi Geolog·cal Survey, 19 9 5' Lingchuan, Sh mxi g Liuquan,;Ling huan, Shanxi yenite diorite Juras ic C Shanxi Geolog·cal Survey, 19 9 Tongguxia-Xil anshan, yenite diorite Juras ic C Shanxi Geolog·cal Survey, 19 9 Lingchuan, Sh mxi ~ Con inned I

Forming Thermal Isoto ic Temp rature Press re Are ock depth gradient Scurces age (~a) (9 ) (GP) (km) ("CIkm) East Longzhen Pingshun-NE Huguan, yenite diorite Juras ic C Shanxi Geolog·cal Survey, 19 9 Shanxi NE Pingshun, hanxi yenite diorite Jurassic C Shanxi Geolog'cal Survey, 19 9 Southeast Ping shun, Shanxi yenite diorite Jurassic C Shanxi Geolog·cal Survey, 19 9 Shuzhangzhen Huguan, Shan i yenite diorite Jurassic C Shanxi Geolog·cal Survey, 19 9 Dabieshan :Juartzmonzonite 170 C Li et al., 2001 Baimajian.Dal:uaping- Dabies an I granite bodies Jurassic C-M Guan et aI., 19 7 Huangshan, Ta.ping, Anbui Jranite 178- 43 C-M Nanjing Unive rsity, 1981 Jingde, Anhui 3ranite 147- 38 C-M Nanjing Unive rsity,1981 Langheqiao, Ji gxian. Anhui Granite 140 C-M Nanjing Unive sity,1981 Fuling, Jixi, A ihui 3ranite 148 C-M Nanjing Unive rsity, 1981 Caoshan, Tong ing, Anhui )iorite 136.6 880- ,240 28-33C 31-37 Du et al., 2004 Jiguanshan, Tongling, Anhui J-ranodiorite 139.8 1,270 1,290 42-48 30-27 Dn et al., 2004 Tongling, Anb i ~lkali-granodiorite L.Jur ssic C-M Wang, 2004 Fanchang-Ton ling Anhui ::!uartz-monzon te Jurassic C-M Lou et aI., 200 Tongling, Anh i yroxene diorit 142.9 C-M Wang et aI., 2004 Jingshan, Huai uan, Anbui oliation Grani 160.2 C-M Xu et al., 2004 Tongguanshan Anhui )iorite in WNV 150 C-M Zhai et al., 1992 Jinkouling, To gling, Anhui J-ranite 136 C Zhou,1989 Tongguanshan Anbui ::2uartzdiorite Jurassic C-M Wang et al., 2002 Xihu, Tongling , Anhui :::luartzdiorite Jurassic C-M Wang et aI., 2002 Hushan, Tongl ng, Anhui ~uartzdiorite Juras ic C-M Wang et aI., 2002 Shizishan, Ton ling, Anbui ~uartzdiorite Juras ic C-M Wang et al., 2002 Dalongshan, Anqing, Anhui Ikali-biotite g anite Juras ic C Jiangxi Geolog ical Survey, 19 3 E'cheng, Hubei 3ranite in WM trend 157.9 C-M Zhai et al., 1992 Tongshankou, Daye, Hubei )iorite in WNV trend 183.2 C-M Zhai et al., 1992 Jinshandian, D ye, Hubei ::!uartz diorite i WNW 138 C-M Zhai et al., 1992 Yinzhu, Daye, Hubei :::luartzdiorite i WNW 189 C-M Zhai et al., 1992 Yangxin, Hubei 3ranodioritein WNW 157- 53 C-M Zhai et aI., 1992 Ruannitu, Yan xin, Hubei )iorite in WNV trend 154 C-M Zhai et aI., 1992 Fengshandong Hubei )iorite in WNV trend 138 C-M Zhai et al., 1992 Jiuliping, Yich ng, Hubei lliyolite Late urassic C Gao et al., 199 Caoguan, west Qinling ~uartz-diorite205 C Li et al., 2004 Donghe, west ::!inling ?yroxene diorit 195.1 C Li et al., 2004 Waquanshan, est Qinling 3abbro 184 C-M Li et al., 2004 Muhuguan, no hQinling J-ranite Jurassic C-M Liu et aI., 199( i0. is' .a Continued :ij e£i Forming Thermal >< Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (km) ("CIkm) ~I Yuku, Luanch an, Henan ranitoid 204 C .§ Shang et al., IJ88 Yinjiagou, Lin bao, Henan anitoid 152 C Shang et aI., I 88 Nannihu, Lu chuan, Henan ranitoid 141 C Shang et al., I 88 i Shangfanggou, uanchuan, Henan ranitoid 134 C Shang et al., I 88

~I Babaoshan, L shi, Henan anitoid JUraS~ic C Shang et aI., I 88 Xiong'ershan, est Henan ranite Juras ic C Hu et al., 2006 Fengshandong Yangxin, Hubtji ranodiorite pOfphyry Juras ic C-M Jiangxi Geolo ical Survey, 19i1n ~~ Jinduicheng.X aoqinling, Shaanxi anite 148 C-M Yan et al., 198 Shanyang-Zha hui, Shaanxi ranite-diorite 148 C-M Yan et al., 198 orphyry Baoji-Longxi , Shaanxi uartz diOriteiranite 187 C Yan et al., 198 Luonan, Shan xian, Shaanxi rano-quartz p rphyry 148 C Shang et al., 1&88 Dongjiangkou, Shaanxi uartz diorite ite 189 C Yan et al., 198 Luonan-Danfe g, Shaanxi , Lushi.Henan iorite, admelli e 173 C Yan et al., 198 Shihuichang, antian, Shaanx dmellite 173 C Yan et al., 198 Huashan, Shaa xi drnellite granite 166 C Yan et al., 198 Mulonggou, H ishan, Luonan Shaanxi iorite 142 C Shang et aI., 1 88 Poxianggou, S aanxi uartz diorite 142 C-M Shang et al., 1 88 Heishan, Luon n, Shaanxi ranodiorite 142 C-M Shang et aI., 1 88 Baijiazhuang, inxian, Gansu dmellite 190 C-M Shang et aI., 1 88 Dongchagou, ansu lkali granite 196 C-M Shang et al., 1 88 Shaoxing Zhej ang ranitoid Jurassic C Yang et aI., 19 6 West Zhejiang ranitoid Jurassic C Yang et al., 19 6 North to Chan hua, Zhejiang ranite 147 C-M Nanjing Unive sity, 1981 Lixi , Wuxing, Zhejiang ranite 145 C-M Nanjing Unive sity, 1981 Fulingxuechu , Lin' an, Zhejiang ranite 143 C-M Nanjing Unive ity, 1981 Dazhang, Fuy g, Zhejiang ranite 140 C Nanjing Unive sity, 1981 Houzhai, Yiw ,Zhejiang ranite 171 C Nanjing Unive ity, 1981 Lishui, Zheji: g anite 163- 74 C-M Nanjing Unive sity, 1981 Shaoxing-Zhuji, Zhejiang ranitoid in NE Juras ic C Yang, 1996 Western Zheji g ranitoid in NE Juras ic C Yang, 1996 Jiande, Lin' an, Jinhua, ZhejiatJg anitoid in NI:1trend Juras ic C Zhu et aI., 200 Coastal areas f Zhejiang-Fujian- ale-Alkali ~imodal155- 39 C Gao et al., 199' Guangdong olcanic Chujia, Ningh i, Zhejiang yolite L. Jurassic C Gao et al., 199' Hutanggang, huji, Zhejiang uff and ignimbrite L. Jurassic C Gao et al., 199' Continued Forming Thermal Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (km) ("CIkm) Zhoucun, JinhE' Zhejiang ff and ignimJrite L. Jutsic C Gao et aI., 199' South Anhui- est Zhejiang anitoid < 14 C Zhou et al., 201M Furong1ing, Z ejiang-Xiangshan Jiangxi ale-Alkali bi oda1 155- 41 C Gao et aI., 199' olcanic Longyou, Zhej] ang uartz-monzonite C Gao et aI., 199' Dayang, Jiand , Zhejiang ranite L. Ju!rsicJur sic C Gao et aI., 199' Suzhou, Jiang u ranite in WNl 155- 41 C Zhai et aI., Chengtou, G yu, Jiangsu type granite in NE L. Jur ssic C-M Li et aI., 199919t Suzhou, Jiang type granite L. Jur sic C-M Zhou et aI., 19 7 Wushan, NW iangxi iorite in WNV 140.1 C-M Zhai et aI., 19 2 Northeast Jian xi ranite porphy 160- 70 C-M Zhou et aI., 20 Dajishan, Jian xi icagranite Juras ic 740 C Jiang et aI., 20 5 Potouzhen, Qu nan, Jiangxi type granite 178 C Chen et aI., 20 Zhaibei, Ding an, Jiangxi type granite 171 C Li et aI., 2003 Quannan, Jian xi type granite C Li et aI., 2003 Xiangshan, Fu hou, Jiangxi type granite C Chen et aI., 19 9 Luoqiao, Shan rao, Jiangxi gnimbrite L.:~~-f7Jur ssic C Gao et aI., 199 Jiujiang-Ruic ang-Dexing iorite in WN trend 204-- 46 C-M Zhai et aI., 19 2 Luxi, Pingxian , Jiangxi ranodiorite po phyry 135 C-M Jiangxi Geolo ica1 Survey, 19 3 Yangchu1ing, uchang, Jiang ranodiorite 142.3 150.6 C-M Jiangxi Geo10 ica1 Survey, 19 3 Dawangmiao, ingxiang, Jianzxi uartz diorite p rphyry 143 C-M Jiangxi Geo10 ical Survey, 19 3 Tongling, Rui ang, Jiangxi ranodiorite po hyry 153 C-M Jiangxi Geolo ica1 Survey, 19 3 Dingjiashan, Jhijiang, Jiangxi ranodiorite po hyry 153 C-M Jiangxi Geo10 ical Survey, 19 3 Chengmengsh , North Jiangxi ranodiorite po hyry 148-~55 C-M Jiangxi Geolo ical Survey, 19 3 Fenglincun, D ngxiang, Jiangxi ranite porph 161 C Jiangxi Geolo ica1 Survey, 19 3 Fujiawu, Dexi g, Jiangxi ranodiorite po 157 C-M Jiangxi Geo10 ical Survey, 19 3 Yongping, Qi shan, Jiangxi ranite porphy 161 C-M Jiangxi Geolo ical Survey, 19 3 Wushan, Ruic ang, Jiangxi ranodiorite po 165 C-M Jiangxi Geo10 ical Survey, 19 3 Bangyankeng, Wuyuan, Jiangxi anodiorite po 155.4 C-M Jiangxi Geolo ica1 Survey, 19 3 Tongchang, D xing, Jiangxi ranodiorite po 170 C-M Jiangxi Geo1o ica1 Survey, 19 3 Baoshan, Wan an, Jiangxi ranodiorite po 176 C-M Jiangxi Geo10 ical Survey, 19 3 Nanmuxiang, ichun, Jiangxi anodiorite 184 C-M Jiangxi Geolo ica1 Survey, 19 3 Qibaoshan, Sh ggao, Jiangxi ranite porphyr 184 C-M Jiangxi Geo1o ical Survey, 19 3

Dong1eiwan, uichang, Jiangxi ranodiorite pothYry JUraS~ic C-M Jiangxi Geolo ical Survey, 19 3 Yongping, Qia shan, Jiangxi iotite admellit Juras ic C-M Jiangxi Geolo ica1 Survey, 19 3 {I Taqian, Lepin , Jiangxi ranodiorite po hyry Juras ic C-M Jiangxi Geo1o ical Survey, 19 3 is ~ Con inned ~ £i Forming Thermal &. Isoto ic Temp rature Press re x Are ock depth gradient Scurces -..J age (~a) (9 ) (GP) (km) ("CIkm) (;l Xihuashan, Da u, Jiangxi lkali granite 184- 48 C Jiangxi Geolog ical Survey, 19 3 .g Huangsha, Yucu, Jiangxi '\lkali granite Juras ic C Jiangxi Geolog ical Survey, 19 3 Tieshanlong, v udu, Jiangxi '\dmellite porp yry, Jurassic C Jiangxi Geolog ical Survey, 19 3 ,I Alkali granite Qianshan, Cho ngyi, Jiangxi '\dmellite, Alkali Jurassic C Jiangxi Geolog ical Survey, 19 3 granite ~ Zhulanmeng, udn, Jiangxi dmellite Jurassic C Jiangxi Geolog ical Survey, 19 3 ~~ nan, Jiangxi u Dajishan, Qua dmellite Jurassic C Jiangxi Geolog ical Survey, 19 3 .g Hukeng, Anfu, Jiangxi vluscovitc gran te 183 Jiangxi Geolog ical Survey, 19 3 C 9­ Xiatongling, F nyi, Jiangxi Muscovite gran te, Jurassic C Jiangxi Geolog ical Survey, 19 3 § 3ranite porphy 0- Xiaolong, Taihe, Jiangxi iotite granite, Jurassic C Jiangxi Geolog ical Survey, 19 3 ;l Jacite porphyry ~ Baishuidong, .ng' an, Jiangxi iotite- muscovite Juras ic C Jiangxi Geolog ical Survey, 19 3 ~ granite Xiangshan, Ch ongren, Jiangxi 3ranite and rhy lite Jurassic C Jiangxi Geolog ical Survey, 19 3 ~ porphyry g Dongjiang, Lo gnan, Jiangxi Biotite -muscov te Jurassic C Jiangxi Geolog ical Survey, 19 3 5· granite Heling, Qings anzhen, NW Ji mgxi lkali granite Jurassic C Jiangxi Geolog ical Survey, 19 3 ,.,.~ Da' anfenshuig an, Jiangxi 3ranite 139 C Ling et aI., 19~9 Wushan, Jiujia g- Ruichang, J iangxi 3ranodiorite po rphyry 140 C-M Luo,2006 ~ inNWW 5· Chengmengsh m, J-ranodiorite porphyry 148 C-M Luo,2006 (jq en Jiujiang-Ruich ng, inNWW Dongleiwan, J ujiang- Ruichar g, Jiangxi J-ranodiorite po rphyry 196 C-M Luo,2006 ~ inNWW g., Baoshan, Jiuji mg- Ruichang, iangxi J-ranodiorite porphyry 176 C-M Luo,2006 ne- inNWW 5· O' Niulingao, G, nxian, Jiangxi 3ranite Jurassic C Jiangxi Geolog ical Survey, 19 3 n Chunyashan, ichun, Jiangxi Biotite and Alk i Jurassic C Jiangxi Geolog ical Survey, 19 3 c g Granite 5· Mengshan, Sh mggao, Jiangxi iotite Granite, Jurassic C Jiangxi Geolog ical Survey, 19 3 g Rapakivi Benggangshan Xinkaishan, D yu, iotite Granite Juras ic C Jiangxi Geolog ical Survey, 19 3

~ 1: Continued 00 Forming Thermal Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (km) ("CIkm) Zengjia1ong, Dean, Jiangxi iotite Granite Jurassic C Jiangxi Geolo ical Survey., 1'183 Xing1uokeng, Ninghua, west flujian iotite Granite, Jurassic C Jiangxi Geolo ica1 Survey. , 1~83 uscovite granite Lingshan, NE hangrao, Jianfi ranite 168 C Nanjing Unive sity, 1981 Fujiawu, Dexi g, Jiangxi anite 161, j57 C Nanjing Unive ity, 1981 Donghengsh , Jiujiang, Jian xi ranite 176 C Nanjing Unive ity, 1981 Five intrusions at West to Jiuji ng ranite 143, 48,155 C Nanjing Unive sity, 1981 Mengshan, Sh nggao, Jiangxi anite 170 C Nanjing Unive ity, 1981 Southwest W, zai intrusion, ichun, ranite 182 C Nanjing Unive ity, 1981 West to Yihua g, Jiangxi ranite 8 C Nanjing Unive sity, 1981 155,11 Nanzhaoxie, L 'an, Jiangxi ranite 183,1 8 C Nanjing Unive ity, 1981 Huangpi, West Guangchang, Jiangxi ranite 164,1 7 C Nanjing Unive ity, 1981 Jiangbei, west ingdu, Jiangx ranite 137,1 5, 175 C Nanjing Unive sity, 1981 Nari'ebo, Nin u, Jiangxi ranite 175 C Nanjing Unive ity, 1981 Xingguo, Jian xi ranite 154 C Nanjing Unive ity, 1981 Zhu1anpu, Hui hang, Jiangxi ranite 136,1 3, 175 C Nanjing Unive sity, 1981 Zhangtiantang Shangyou, Ji~gxi ranite Juras ic C Nanjing Unive ity, 1981 Hongtaoling, hongyi-Shang ou, ranite Juras ic C Nanjing Unive sity, 1981 Xialong, Chon yi- Shangyou, Jiangxi ranite Juras ic C Nanjing Unive sity, 1981 Tianmenshang SE Chongyi, J angxi ranite Juras ic C Nanjing Unive ity, 1981 Piaotang, nort Dayu, Jiangxi ranite 161 C Nanjing Unive sity, 1981 Bai'e, south Yi du, Jiangxi ranite Juras ic C Nanjing Unive sity, 1981 Tieshikou, sou h Xinfeng, JiJXi ranite Juras ic C Nanjing Unive ity,1981 South Longn ,Jiangxi ranite Juras ic C Nanjing Unive sity, 1981 Wuliting, Daji han, Quannan, iangxi ranite 158,1 0 C Nanjing Unive ity, 1981 Youshan, SE ayu, Jiangxi ranite 177 C Nanjing Unive ity, 1981 West Xunwu, iangxi ranite 164, 89 C Nanjing Unive sity, 1981 NoA14 Minin , wugongShan:J.JiangXi ranite 165,1 6 C Nanjing Unive ity, 1981 Hongshuizhai, Chongyi, Jiang i anite 188- 40 C Nanjing Unive sity, 1981 Yushan,Gulon gang, Xingguo Jiangxi ranite 146- 75 C Nanjing Unive ity, 1981 76 intrusions i Shangrao, Ji gxi ranitoid in NJtrend Juras ic C Zhu et al., 200 Nanxi, Jitai, Ji ngxi 1kali basalt 139- 43 C-M Yu,2005 Shangqinggon , Guixi, Jiangx agu1ing Form lion, L. Jur sic C Gao et al., 199' Volcanic rock Xiangshan, Chongren, Jiangxi huling Formation, L. Jurassic C Gao et al., 199' Volcanic rock i0. is' .a Continued ~ £i &. Forming Thermal x Isotopic Temperature Press~re Are ock depth gradient Sources -..J age (*a) C'(:) (GN) (km) ("CIkm) (;l Southern Jiangxi hangpu and Ji Jurassic C-M Lai et al., 199( .g longzhang F!ation, volcanic ,I 398 bodies in athysian plate ranitoid in N trend L.JU~SiC C Zhu et al., 200 Zhenghe, Fuji n anitoid Juras ic C Yang et al., 19 6 Fangken,Yong ing, Fujian type Basalt M. J assic C-M Zhou et al., 20 5 ~ Guangze, Fuji n ranite 180 C Ling et al., 19 9 ~~ u Wuping, Fujia anite 166 C Ling et aI., 19 9 .g Xiaotao.Yong' n, Fujian ranite 180 C-M Ling et al., 19 9 9­ Yongding, Fuji an ranite 145 C-M Ling et al., 19 9 § Hukeng,Yong ing, Fujian dmellite 165 C Ling et aI., 19 9 0- Bailian, Jiangl , Fujian ranite 140 C-M Ling et al., 19 9 ;l Guiyang, Yon chun, Fujian dmellite 201 C-M Ling et al., 19 9 ~ Zhenghe, Fuji n ranite 140 C-M Ling et aI., 19 9 ~ Youxi, Fujian ranite 140 C-M Ling et al., 19 9 Zhongteng,Pin he.Pujian onzonite-diorite 136 C-M Ling et al., 19 9 ~ Maotiling,Son xi, Fujian desite L. Jur ssic C Gao et aI., 199' g Huyang, Shan hang, Fujian ranite L. Jur sic C Gao et aI., 199' 5' Longmen. An i, Fujian ranite L. Jur ssic C Gao et aI., 199' Damaoshan, L nghai, Fujian ranite-admellite L. Jur sic C Gao et aI., 199' ,.,.~ Jinshan, Anxi, Fujian ranite-admellite L. Jur sic C Gao et aI., 199' Gaide, Dehua, Fujian ranite L. Jur ssic C Gao et aI., 199' ~ Yongfu,Zhang ing, Fujian ranite L. Jur sic C Gao et aI., 199' 5' Gumeishan.Fu ing, Fujian dmellite L. Jur sic C Gao et aI., 199' (jq en Longsandong, hao'an, Fujiar ranite-admellite L. Jur sic C Gao et aI., 199' Hufang, Ming i, Fujian ranite L. Jur sic C Gao et aI., 199' ~ Caixi, Shangh ng, Fujian dmellite L. Jur sic C Gao et aI., 199' g., Dabugang,Sha wu, Fujian ranite L. Jur sic C Gao et al., 199' ne- Southeast Puc eng, Fujian anite Juras ic C Nanjing Unive sity, 1981 5' cc Southeast Nan ing, Fujian ranite Juras ic C Nanjing Unive ity, 1981 n North to Shaxi n, Fujian ranite Juras ic C Nanjing Unive ity, 1981 c g Xingluoken, Qingliu, Fujian iotite Granite 155 C Nanjing Unive sity, 1981 5' North to Qingl u, Fujian ranite C Nanjing Unive ity, 1981 g Gutian,Longq an-Liancheng, ranite 173- 46 C Nanjing Unive sity, 1981 Hetian, SE Ch ngting, Fujian anite 148 C Nanjing Unive sity, 1981 Guobao, Dehu , Fujian ranite 157- 60 C-M Nanjing Unive ity, 1981 £ Continued Forming Thermal Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (km) ("CIkm) Zhongteng, Pi ghe, Fujian ranite Juras ic C-M Nanjing University, 1981 Nandayang, L ngyan, Fujian anite 158 C Nanjing University, 1981 Zhenghe, Fuji ranitoid in 3Etrend Juras ic C Yang, 1996 Coastal zone 0 Fujian ndesite-rhyoli e L. Jur sic C-M Jiang, 2001 Lingdai, Xian ia, Fujian rachyte-rhyoli e L. Jur ssic C-M Jiang, 2001 Yongding, Fujian imodal vole crocks 188- 79 C-M Gao et al. 199' Gutianxian, F "ian ranoid 164- 43 C-M Gao et al., 199' Xing1uokeng, inghua, Fujian anoid 164- 43 C-M Gao et al. 199' Longsandong, hao'an, Fujiar ranitoid 164- 43 C-M Gao et al. 199' South wuyishr n, Fujian ranitcid 164--143 C-M Gao et al., 199' Dawangshan, inghe, Fujian ranitoid 164-- 43 C Gao et al. 199' Hongshan, Fu hou, Fujian uartz syenite 135 C Gao et al. 199' Daiyunshan, ehua, Fujian gnimbrite L. JUf ssic C Gao et al. 199' Lianhuashan, nxi, Fujian 'off and Andesite L. Jur ssic C Gao et al. 199' Mei1in, Nanjin , Fujian gnimbrite L. Jur sic C Gao et al. 199' Shiping, Chan le, Fujian gnimbrite L. JUf ssic C Gao et al. 199' Bu1ing, Minho , Fujian gnimbrite L. Jur ssic C Gao et al. 199' Yangzhong, Ningde, Fujian L. Jur sic C Gao et al. 199' Nankou, Jiang e, Fujian 83 gi~::~~~mellr',e 187- C-M Gao et al. 199' Jiufeng, Pingh , Fujian acite L. Jur sic C Gao et al. 199' Yangmingshan Taihei, Taiwar ranite-porphy L. Jur sic C Gao et al. 199' Tianzhushan, etween Chong'~n,Fujian and iranite 168 C Nanjing University, 1981 Qianshan, Jian xi Dajishan, Jian xi ranite 15L7 144 C Zhang et al., 2 06 Qingzhang, S th Nanxiong, uangdong ranite 185 C Nanjing Unive ity, 1981 Lianhuashan, aoping, Guang ong ranite-porphy L. JUf sic C Gao et al. 199 Beidiaogong, aifeng, Guang ong ranite 157 C-M Nanjing Unive sity, 1981 Dongzhongba, Zijin, Guangdo g ranite 157- 45 C-M Nanjing Unive ity, 1981 Beitouwo, Puning, Guangdon anite 143- 47 C-M Nanjing Unive sity, 1981 Nangudoush , Taishan, Gu gdong ranite 148 C-M Nanjing Unive ity, 1981 Guanghai, Tai han,Guangdon ranite 166- 67 Nanjing Unive ity, 1981 Shanbeishan, aishan, Guang ong anite 136- 39 C-M Nanjing Unive sity, 1981 Putang, Yangji g, Guangdon ranite 157- 62 C-M Nanjing Unive ity, 1981 Dianbaitangko , Yangjiang ranite 140- 48 C-M Nanjing Unive sity, 1981 Guling, West eyuan, Guang'10ng anite 143- 63 C-M Nanjing Unive sity, 1981 {I Northwest Xin eng, Guangdorig ranite 160 C-M Nanjing Unive ity, 1981 is ~ Continued :ij £i Forming Thermal e Isotopic Temperature Pressure >< Are ock depth gradient Sources age (*a) C'(:) (GP~) (km) C'CIkm) ~I W Heyuan, S ingde, Guangdong ranite 165 C-M Nanjing University, 1981 .§ Lianhe, Hetai, uangdong iotite granite 186 942.61-953 C Wu,1986 Gaocun, Hetai Guangdong egmatite 194 C Ye,1989 i Zacun, Hetai, uangdong iotite admellin 157.5 C-M Cui, 1989 Tangkou, Gua gdong anite 135-~61 C Wanget al., 2 ~I Xituokou, Gu gdong ranite 150 C Wang et al., 2 Mashan,west uangdong ranite 201 C-M Wang et al., 2 ~~ Gangrnei, Gu gdong anite 172-~86 C-M Wanget al., 2 Fougang, Gua gdong ranite 141 C Nanjing Unive ity,1981 Guidong, Gu: gdong ranite 143 C Nanjing Unive sity, 1981 Shibei, Lianpi g, Guangdong ranite 165 C-M Nanjing Unive ity, 1981 West to Liann n, Northwest tjTaibaO ranite 168 C Nanjing Unive ity, 1981 Shantou, Guan dong ranitoid in NE C Yang, 1996 Zhenjiang,Sha guan City, Gu ngdong ranite C Gao et al., 199' Nanling, west uangdong ranite C Geng et al., 20b6 Nanling, south China drnellite C Hua,2005 East to Ganji g, Nanling cid volcanic C Hua,2005 Eastern Nan1i asalt Lava L Zhang, 2004 Eastern Nanli yke L Zhang, 2004 Zhuguangshan drnellite C-M Ma et al., 200t Tabei, Eastern anling type syenite C-M Chen et al., 20~ Potou, Eastern Nanling ranitoid L Chen et al., 20 Fogang, west uangdong type granite <\nd C-M Geng et al., 20 6 yenite Nanling, Southeast Hunan ranodiorite 170 C-M Geng et al., 2096 Shizhuyuan, Chengzhou, Hunan iotite admellite, Jurassic C Jiangxi Geological Survey, 19$3 ranite porphy Baofengxian, outheast Hunar iotite admellin 156.8 C Jiangxi Geological Survey, 19$3 Shaziling, Xia gtan, Hunan type granite 184 C Gilder et al., 1~96 Jinjiling, Lans an, Hunan type granite 156 C Fu et al., 2005 Qianlishan, C enzhou, Hunan type granite 152 C Li et al., 2004 Huziyan, Dao ian, Hunan erzolite in basalt 85-38, L 132j151 Kong et al., 20~1 Liujiazui, Hu ong, Hunan ranite 165 C-M Nanjing Unive ity, 1981 Mufushan, bo ndary of Hun~Hubei ranite 138- 40 C Nanjing Unive sity, 1981 Jiuningshan, S Lanshan, Hu an anite 157 C Nanjing Unive sity, 1981 Xianghualing, orth Linwu, H nan ranite 155 C Nanjing Unive ity, 1981 Con Inned Forming Thermal Isotopic Temperature Pressure depth gradient Area Rock age (Ma) (OC) (GPa) Sources (Ian) ("CIkm) Yaogangxian, south Zixing, Hunan Granite 177-178 C Nanjing Unive sity,1981 Qianlishan, Dongpo, Hunan Granite 139-172 C Nanjing Unive sity,1981 Tongshanling, liang- yong, Hunan Granite 176 C Nanjing Unive sity,1981 Ziyunshan, Xiangxiang, Hunan Granite 147 C Nanjing Unive sity,1981 Nanyue, Hengyang, Hunan Granite 178-153 C Nanjing Unive sity,1981 Dengbuxian, north Chaling, Hunan Granite Jurassic C Nanjing Unive sity,1981 Zhuguangshan, Rucheng, Hunan Granite 172 C Nanjing Unive sity,1981 North Zhuguangshau, Xitian, Hunan Granite 177 C Nanjing Unive sity,1981 Guidong, SE Zhuguangshan, Hunan Granite 170-175 C Nanjing Unive sity,1981 NE Dupangling, Daoxian, Hunan Granite 170-175 C Nanjing Unive sity,1981 Jinjing, SE Pingjiang, Hunan Granite 168 C Nanjing Unive sity,1981 Taiyangshan, Ningyuan, Hunan lherzolite in basalt Jurassic C-M Chen et al., 201/4 NW Guposhan, Hezhou, Guangxi Granite 164-160 C Gu et al., 2006 East of NW Guposhan, Hezhou Granite 150-146 C Gu et aI., 2006 West of NW Guposhan, Hezhou Granite 150-146 C-M Gu et al., 2006 Huashan, Nanning, Guangxi A type granite 161-165 C Li et al., 2004a Yangmei, Rongxian, Guangxi A type granite 161.6 C Li et aI., 2004a Lisong, Hexian, Guangxi A type granite 160 C Li et al., 2004a Qinghu, Luchuan, Guangxi A type granite 158 C Li et al., 2004a Yuanshishan, north to Pingle, Guangxi Granite 153 C Nanjing Unive sity,1981 Limn, southeast Guilin, Guangxi Granite 185-172 C Nanjing Unive sity,1981 South Miao'ershan, Guangxi Granite 160-180 C Nanjing Unive sity,1981 Luorong, Southeast Guangxi Gabbro-diorite-mo- Jurassic C-M Guo et al., 200 nzonite-syenite Mashan, Southeast Guangxi Alkalic Gabbro- Jurassic C Guo et aI., 200 syenite-Granite Yuxi, Yulin City, Guangxi Rhyorite L. Jurassic C Gao et al., 199 Guposhan, Guangxi Granitoid L. Jurassic C-M Wang et aI., 20P6

Sichuanian Period 135-56 Ma North Dabieshan coal metamorph. 129 191 5.8 32.7 Zhang, 2001 Shan-DanQinling Mylonite 126 530 0.65 21.7 24.4 Zhou et aI., 19 6 Chifeng Anphibo1ite 133 550 0.54 20 27.5 Zhang et aI., 2 /02 Yuli, Taiwan Green schist Cretaceous 500 0.8 26.7 18.7 Chen et aI., 19 4 Tailuge, Taiwan Anphibo1ite 87 600 0.6 20 30 Chen et aI., 19 4 {I Tailuge, Taiwan Sillimanite 87 600 0.5 16.7 35.9 Cao et al., 199 is ~ Con inued :ij £i Forming Thermal e Isoto ic Temp rature Press re >< Are ock depth gradient Scurces age (~a) (9 ) (GP) (km) ("CIkm) ~I Tengchong 3ranulite 60-75 860 I 33.3 25.8 Ji,1998 .§ West Yunnan 3ranulite 75 860 I 33.3 25.8 Zhong et aI., I 99 Nyainqentangl a J-reen schist ~65 610 0.5 16.7 ~36 Xizang Geolog icel ~65 ~38 i Nyainqentangl a J-reen schist 650 0.51 17 Survey, 1993 Daqing oil fiel oal metamorpb. E.Cre aceous reflec ivity 6D-30 Wu et aI., 199 ~I Songhuajiang- iaohe basin andstonc-shale L.Cre aceous of co 42-48 Ren et aI., 200 Santanghu bas n andstone-shale Creta eous reflec ivity ~22 Zhou et al., 19 8 ~~ Hongze, Jiang u andstone-shale Paleo ene of co I 36-40 Zhou et al., 19 8 Erenhot basin andstonc-shale E.Cre aceous reflec ivity ~49.6 Ren et aI., 20C) West Sichuan andstone-shale ~60 of co' I ~25 Liu et aI., 199 Kalpin, Xinjiai g andstone-shale Creta eous 15-17.7 Wei et aI., 198 Tarim basin andstonc-shale Creta cous reflec ivity 25 Fan et al., 199 Song-Liao bas n andstone-shale Creta eous of co' I ~38 Wang et aI., 1989 Erdos basin andstone-shale Creta eous 33-45 Ren et aI., 199 Huanggangliar g-Ganzhue en iao, Dahing- 3ranoid in NNI trend Creta eous CoM Xiao et aI., 20(14 ganling Northern Dahi gganling :Iigh potassiu n calc- L. Cr taceous C Yin et al., 200! ilkali series Northern Dahi gganling Ikali-subalkal' E.Cr taceous C-M Yin et aI., 200 Balinzuoqi, M d.-S. Dahingganling 3ranite 115- 17 C-M Xue et al., 200 Shuanfatun, M u..s. asalt 121.9 CoM Laofangshen, Wushijiazi, mi die Dahing- 3-ranite 127- 36 C-M Xue et al., 200 ganling Haolaibao, Ba ridongshan, 3ranoid in NNI trend Creta eous C Xiao et aI., 20(14 Inner Mongoli Gongnongbing, Lubei, Inner 1\ ongolia Rhyolite 114.2 C Chen et al., 19 7

Baiyinbaolihac , Lubei, Inner ~ongolia ruff, rhyolite 121.3 C Chen et al., 19 7 md andesite Chabugan, Tia shanxian, lone Mongolia hyolite 124 C Chen et al., 19 7 Chabugan quarry, Tian-sha xian, Inner uff and 126.5 C Chen et al., 19 7 Mongolia rachyandesite Heilongtan, K' aqin, Inner M ngolia Jlivine minette 124 CoM Shao et al., 20 3 Chifeng, Inner Mongolia asaltin NNE 107.3 CoM Zhang et al., 2 03 Qingshankou ormation, Song liao basin Iholeiite in E. Cr taceous CoM Lu et al., 1997 'lNE trend Jiutai, Jilin )acite Creta eous 1,276 1.27 42C-M Lu et al., 1996 Continued

Fonni g Thermal Iso opic Te perature Pr ssure Area Rock depth gradient Sources age (Ma) ("C) « Pa) (km) ("C/km) Jiutai, Jilin Dacite inNN Cre aceous 70-80 Lu et al., 1 96 Hafucun, Sipi g, Jilin Rhyolite 122 C-M Chen et aL 1997 Changchunda im Yitong-Dat n, Jilin Basalt 92. C-M Zhang eta .,2006 Fufengshan, ( ~angchun,Jilir Alkali olivine basalt and 82. -83.5 L Liu,1992 tholeiite Siziwangqi, It ner Mongolia Granulite 108 6-128.4 C-M Xu et al., 2P04 Sanmen, Sipi g, Jilin Mantle inel sian in 110 1 1,1 0 4.5 9.1 150-3 OL 7-4 Zhang, 20 1 Rhyolite Fuxin, Liaoni g Peridotite 84. 1,2 2 2.9~ 97.7 13 Zheng, 19 9 Jianguo, Fuxi , Liaoning Mantle intrus on in A 109 93 C-M Zhang eta .,2003; type granoid Shao et al. ,2004 Yemaotai, Zh ngwu, Liaonin Trachyandesit andesite 1248 L Chen et aL 1997 Dingjiafang,Z angwu, Liaonirg Dacite 1259 L Chen et aL 1997 Yingzi, Huide Liaoning Trachyandesit dacite 1237 L Chen et aL 1997 Maoniuhai, Z angwu, Liaoni g Andesite 1255 L Chen et aL 1997 Daheishan, B .piao, Liaoning Dacite, rhyolite 88. L Chen et al. 1997 trachyandesite Hejiagou, Yix an, Liaoning Andesite 119 L Chen et aL 1997 Zhujiagou,Yi .an, Liaoning Andesite 1245 L Chen et aL 1997 Sanbailong,Yi ian, Liaoning Andesite 1255 L Chen et aL 1997 Zhuanchengzi Yixian, Liaon 'rg Andesite 129 L Chen et al. 1997 Shangdijiagou Yixian, Liaon ng Andesite 133 L Chen et aL 1997 Yixian, Liaoning Basalt-andesit Cre ac. 1,1 7 0.Op2 67 L 17 Zhang et a .,1994 Damintun, La Iver Liaohe Basalt in NNE 74. C-M Liu,1992 Fuxin, Liaoni g Basalt in NNE 94. C-M Zhang et a .,2003 Zhangwu, Lia ning Trachyandesit in NNE 124 117 C-M Hong et al. 2003 trend Yixian, Liaoning Basalt in NNE Cre ac. C-M Hong et aL 2003 Fushun, Liaon ng Tholeiite 52. 9-72.02 L Liu,1992 Yangmaying, heling, Liaoni g Andesite, rhy lite 135 C-M Chen et aL 1997 Nankou, Beiji g Olivine basalt 128 C-M Hong et al. 2003 Nankou, Beiji g Alkali Basalt and gran- 119 114 M Shao et al., 2001 ite dyke in N!' W trend Xuejiashiliang ' North Beijing Gabbro and s enite 132 8-123.3 C-M Su et al., 2 06 {I Fangshan, Bei ing Grano-diorite 1307 M Cai et al., 005 is ~ Continued :ij e£i Forming Thermal >< Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (km) ("CIkm) ~I .§ Nankou, Beiji!g amprophyre dia- 119-~14 C-M Shao et al., ZO(])I ase r Kongdian-Hua ghua, Dagang il Field 'rachyandesite 65-7 C-M Compiling Gr up of petrol.lGeol., i 1993 Section I-Z, ongdian Fonnton, Dagang amprophyre t'n NE Eocene L Compiling Gr up of Petrol. Geol., ~I oil field 'end 1993 Taihangshan Quartz Syenite NE IZ7-~33 C-M Chen et aI., ZO 6 ~~ Well Bai 4, Zh gqiang 'rachyandesite 98.Z C-M Chen et al., 19 7 Well Bai 5, Zh gqiang 'rachyandesite 109.1 C-M Chen et aI., 19 7 Well Bai 8, Zh gqiang rachyandesite 8004 C-M Chen et aI., 19 7 Well Bai 10, Z angqiang 'rachyandesite 105.Z C-M Chen et al., 19 7 Haoying, Lu ing, Hebei ndesite 116.Z Z0-4OC Wu,1984 North to Chan Ii, Hebei ranite 134.1 C Wu,1984 Pingquan, Heb i desite 13 Z0-4OC Wu,1984 96.8-1 Shimengou, C engde, Hebei ndesite 113- 14 Z0-4OC Wu,1984 Manziying, Qi n'an Hebei ndesite 109.8 Z0-4OC Wu,1984 Lingyuan-Jian hang, North H.ebei asalte-andesite in IZ0- 35 C Lu et al., Z005 NE trend Zhang et aI., Z(])03 Taihangshan, ~rthChina amprophyre L. M1S0ZOic M Weideshan-H yang,E Shangd ng ranite L. Cr tac. C-M Sun, 1994 Cuokou-Laosh n,East Shangd ng ranite L. Cr taco C-M Sun, 1994

Denggezhuan ore deposit, E~tShangdong ~yliteinclusion in Tra­ 80-1 9 C-M Chen et aI., 1993 hyte and alkalifbasalt

Zhucheng, Ea~Shangdong kali -basalt 76 L Meng et al., Z~06 Jiaozhou, East Shangdong kali-basalt 72 C-M Meng et aI., Z 06 Daxizhuang, st Shangdong asalt with IheJ:lite 73.Z 1,0101-1,140 Z 50-70 L 18.5 Yan et al., ZOO b Eastern Shand ng amprophyre yke in 110-]05 C-M Chen et aI., 19 3 NE asic dyke in IZ0-~30 C-M Eastern Shand~g Zhang et aI., ZiOZ Qingshanzhu i Shandong desiteinNN IZ7 C-M Chen et al., 19 3 Fangcheng, Sh dong asaltin NNE IZ4.9 C-M Zhang et al., Z 03 Zouping, Shan ong abbroinNNE 115 C-M Hong et aI., ZO 3 Zhucheng, Sh ndong livine basalt tn NNE 111.4 C-M Hong et aI., ZO 3 rend

Daxizhuang, northeast Jiaozhou, Shandong .....herzolite inelu ion Cretac. 970-],140 Z.O 65 L 17 Yan et al., ZOO Daxizhuang, NE Jiaozhou, Shandong Basalt 73.5 65-95 L Yan et al., ZOO Continued

Forming Thermal Isotopic Tem~raturePress1re Are ock depth gradient Sources age (*a) () (GP) (km) ("CIkm)

Hanqiao, QiXi~Shandong ndesite 119.4 20-40C Wu et aI., 198 Chenjiayu, Lai u, Shandong ndesite 121 20-40C Wu et aI., 198 Xidong, Zoupi g, Shandong ndesite 106.5 20-40C Wu et aI., 198 Guojialing, Zh oyuan, Shandong rano-diorite 130-126 C-M Liu,2006 Mengyin, Sha dong Ikali basalt In NNE 124-115 C-M Zhang et aI., 2r3 end Jinan, Shand0 abbro in NNE 115 C-M Hong et aI., 20 3 Dongliujing, ozhuang, SW $handong ano-diorite 127 C-M Xu et aI., 2004 Tietonggou, L iwu, Shandong unite in dorite 119-132 L Xu et aI., 1993 Jinling, Zibo, handong unite in diorin 119- 1132 L Xu et aI., 1993 Feixian, Shan ong antle sourc relict 119 L Pei et aI., 201M 1 rystal Western Shandong 'yroxene inelJ sian in Cretaceous L Wang et aI., 2r abbro-diorite

Aishan-Huash~'Shangdong ranite in SN L. cr~taceous <0.11 C-M Sun, 1994 Yuangezhuang Yashan, E. Shangdong ranite L. Cr taceous C-M Sun, 1994 Tongjing, Yin , Middle Shandong iorite porptry in 125- 17.5 C-M Wan et aI., 19 2 NE trend Jinchang, Yinan, Middle Shandong ranite porp yry in 105.4 C trend South Pingshu , Shanxi yenite-diorite 123-~26 C Luoting coal Ii Id, Guangling, Shanxi iabase 134.5 C Julepu, Daton , Shanxi iabase 116.3 C Northeast Yet u, Linchuan, S anxi yenite-diorite Earlyjcretac. C-M West to Liuqu n, Linchuan, S anxi yenite-diorite Early Cretac. C-M Tonggujiacun, ortheast Line an, Shanxi yenite-diorite Early Cretac. C-M Shadizhan-Do gqiao, south to Pingshun, yenite-diorite 123- 26 C-M Shanxi East to Longz en, Pingshun, hanxi yenite-diorite Early Icretac. C-M Shanxi Geolog·cal Survey, 19f Northeast 5 to Pingshun, S anxi yenite-diorite Early Cretac. C-M Shanxi Geolo 'cal Survey, 19 3 Southeast Pin shun, Shanxi yenite-diorite Early Cretac. C-M Shanxi Geolog·cal Survey, 19 3 Shuzhangzhen southeast Hug an, Shanxi Early Cretac. C-M Shanxi Geolo ·cal Survey, 19 3 ~::::-diOrite Xigou, Luona , Shaanxi 124.5 C Yan et aI., 198 Daijiatan, Ziy g, Shaanxi ranite, Rhyolite por- 129 C Yan et aI., 198 hyry {I Jinduicheng, Huaxian, Shaanx ~ranite-porphy 132 C Shang et aI., IJ88 is ~ Con inued :ij £i Forming Thermal e Isoto ic Temp rature Press re >< Are ock depth gradient Scurces age (~a) (9 ) (GP) (km) ("CIkm) ~I

Shangxian, Sh anxi ~uartzdiorite, ranite 114- 33 C Van et al., 198 .§ Huashan Mou t, Huayin, Shas nxi 3ranite 100- 13 C-M Van et al., 198 West Qinling asalt, A type L.Me sozoic C-M Li et al., 2006 i Heyu, Luanch an, Henan 3-ranite 110 C Shang et al., I 88 Laojunshan.Luanchuan, Rena 3ranite 105 C Shang et aI., I 88 ~I Jinzhai-Suxian hi, North Dabi shan )iorite, granite onzon- 140-\7 866- ,150 O.I--D2 30 29-38 Li et al., 1997 te ~~ North Dabiesh n typeTTG gni ss 130- 20 C-M Li et al., 2001 North Dabiesh n 7roxene gabbr 130- 20 C-M Li et al., 2001 Tiantangzhai, abieshan Granitoid 131 830 0.54 18C 46 Wang et aI., 2000 North Huaiyan asalt in WNW Early Cretac- C-M Lu et aI., 2005 eous North Huaiyan rachyandesite n Early Cretac- C-M Lu et aI., 2005 WNW trend eous Dabieshan 3-ranitoid 125-55 C Ma et al., 1999 Mingguang, Ji shan, Anhui )livine basalt 72.2 L Liu,1992 Tieshan, East ubei )iorite in NNE 117± 0 C-M Zhai et aI., 1992 Jiangling, Hub i Fholeiite 57-75 L Liu,1992 Guangqi-Huan mei EasternH bei yenite-Alkali ranite 125 C-M Zhai,1989 Lingxiang, Da e, Hubei Rhyolite 115-50 C Wu et al., 198 Taihezhen, E' cheng, Hubei lliyo1ite and pe arlite 96-1 2 C Wu etal., 198 Lingxiangzhen, Daye, Hubei asalt 114- 27 L Wu et aI., 198 Jiuhuashan, so thAnhui dmellite 123 C Zhang et al., 2 02 Huangshan, so thAnhu dmellite 125 C Zhang et aI., 2 02 Tanshan, south Anhui 3ranite 124 C Zhang et aI., 2 02 Wuling, south Anhui ::;ranite 129 C Zhang et al., 2 02 Tongxinguo, S nth Anhui :;luartz Syenite 127 C Zhang et aI., 2 02 Fuling, south nhui 3-ranite 121 C Zhang et al., 2 02 Yanghutang, Anhui Gabbro 125 C-M Xing et al., 19 4 Huoli, Anhui ::;ranite 123 C-M Xing et al., 19 5 Longwangshar , Nanjing-Wuh rachyte-andesi e 126.1 C-M Li et al., 1998 Niangniangsh: n, Nanjing-Wu u honolite 99.8 C Wu et aI., 198 Meishan, Nanj ng-Wuhu ndesite and tr chyte 91-1 4 C Wu et al., 198 Tongjing, Nan ing-Wuhu amprophyte 105 C Wu et aI., 198 Yueshan, Anh i )iorite in NNE 80± C-M Zhai et aI., 1992 Hongzhen, An ui ::;ranite in NNE 124 C-M Zhai et al., 1992 :jl Continued

Forming Thermal Isoto ic Temp rature Press re Are ock depth gradient Sources age (~a) (9 ) (GP) (km) ("CIkm) Gushan, Nanjing-Wuhu ndesite 115.7 C Wu et al., 198 Fenghuangshan, Anhui }ranD-diorite .n NNE 133 C-M Zhai et al., 1992 rend Washan, Ma'anshan, Anhui )iorite porphy 'Y dyke 120 C-M Zhai et al., 19d2 nNNE Huaiguang, BJbU' Anhui J-rano-diorite 130 C Jin et al., 2003 Nvshan and L shan, Benbu, ~nhui J-ranite 129- 30 C Yang, 2005 Dongguandian Benbu, Anhui }rano-diorite 126.9 C-M Xu et al., 2004 Jiaohuashan,H angshan, Anh i 3ranite 125 C-M Wang et al., 2~5 Zhangbaling, nhui ndesite 126 C-M Niu,2006 Niangniangsh ,Anhui type granite 97 C Xing et al., 19 9 Lishui, Jiangsi )iorite porphy 'Y dyke 124-\ 9 C-M Zhai et al., 19 2 nNNE Maotan, GUic~"Anhui ~ type granite 99 680-~50 L Wu et al., 199 Huangmeijian, Congyang, Anhui ~ type granite 133 C Zhang et al., 1~88 Kedoushan, F' chang, Anhui asa1t Late retaceous L Yan et al., 200~a Fanchang, N [ing-Wuhu )iorite-alkaligr nite- 120- 10 C-M Qi et al., 2002 asalt-rhyolite LUjiang_ZOngJng, Anhui 120- 10 C-M Qi et al., 2002 Tiantangzhai, abieshan 3ranotoid in Nl ffi 131 830 0.54 18C 46 Wang et al., 2qoO Dabieshan 3ranotoid 125-\5 C Ma,1999 Liguo, north zhou, Jiangsu )iorite porphyr 131 C-M Xu et al., 2004 Northwest Suz au )iorite porphyr; 132 C-M Xu et aI., 2004 Nanjing-Wuhu )iorite porphy y dyke 136-\ 1 C-M Zhai et al., 19'12 nNNE ~ type granite E. Cr tac C Zhou et al., 19?7 Suzhou, Jiangl Suzhou, Jiang u ~ type granite 133- 23 C Chen et al., 1993 Jiashan, Chen tou, Ganyu type granite in NE E. Cr taceous C-M Li et al., 1999 Funiushan, Zh ngjiang, Jiangsu }ranD-diorite 111 C-M Yeet aI., 1999 Shima, Jiangs )iorite in NNE 95.5 C-M Zhai et aI., 19~ Yongjia-Leqin ,Zhejiang lliyo1ite 91.4- 13.1 C Gong et al., 19 8 Yongjia-Leqin ,Zhejiang lliyo1ite, trach te, an- Early Creta- C-M Gong et al., 19 8 esite, basalt ceous Luannitan, C~stof SE China 3ranite 124 C-M Li et al., 1998 Honggong, Zh Jiang :;Juartz Syenite 123 C-M Chen, 1991 {I Tiantaishan, Zhejiang Ika1i Granite 114 C Zhang et al., 2liJ02 is ~ Continued :ij e£i Fonning Thermal >< IsojOPiC TeIj1perature Pr~ssure Are Rock depth gradient Sources age (Ma) ("C) «(1Pa) (km) ("C/km) ~I .§ Dalishan, Notwest Zhejiang Alkali Granite Early Cretaceous C Zhang et~." 2002 Bashan, North est Zhejiang Alkali Granite 110 C Zhang et ., 2002 Sucun, Suich g, Zhejiang Alkali Granite 86 C-M Wang et aI , 2005 i East Zhejiang Tuff 130 86t 0.61 20C 43 Wang, 198 West Zhejiang Tuff in NE trehd 130 100 70 0.6 20C 35 Wang, 198 ~I West Zhejiang Granite in NE ere t100aceous C Yang et al. 1996 ~~ Changshan, Z ejiang Rhyolite porp~yry124 C Wu et aI., 984 Chayuan, Zhe iang Rhyolite porp yry 133 C Wu et aI., 984 Jinhua, Zheji g Rhyolite porp yry 133 C Wu et aI., 984 Changle, Che xian, Zhejiang Granite 132 C-M Nanjing U iversity, 1981 Qingjubao,Sh ichang Granite 120 C-M Nanjing U iversity, 1981 Wuxi, Yunhe, hejiang Granite 124~95 C-M Nanjing U iversity,1981 Quanyantou, enzhou Granite 90 C-M Nanjing U iversity, 1981 West Pingyan , Zhejiang Granite 72 C-M Nanjing U iversity, 1981 Qingjie, Ping ang, Zhejiang Granite 76 C-M Nanjing U iversity, 1981 Tangyuankou, Jiangshan, Zhejiang A type granite 124 C Chen et aI. 1991 Qingtian, Zhejiang A type granite 101 C-M Qiu et al., 999 b Putuo, Zhous , Zhejiang A type granite 94 C-M Qiu et al., 999 b Taohua, Putuo Zhejiang A type granite 93 C-M Qiu et al., 999 b Putuo, Zhous , Zhejiang Diorite and alkali gran­ 92-b1.8 C-M Qiu et al., 999 b ite

Taohua ISlandf,coastalOf Zhejiang Alkali granite 90.~3-142.4 C-M Qiu et aI., 1999 b Qingtian, Zhej" ang Alkali granite 1007-114.3 C-M Qiu et al., 999 b Zhejiang-Fuji -Guangdong A type graniteIin NE 100 70 C-M Hong et aI. 2002 Liangnong, Yi yao, Zhejiang Granite-syenit 128 103 L Gao et al., 999 porphyry-gabbro Beijie, Shuich g, Zhejiang Alkali granite 86 C-M Wang et aI , 2005 North Changp ,Fujian Granite C-M Nanjing U iversity, 1981 Shao'an, Ch: gpu, Fujian Granite creiceousere aceous C-M Nanjing U iversity, 1981 Yunxiao, Fuji n Granite with arnazonite 100 112 C-M Nanjing U iversity, 1981 Dongshan lsi d, Fujian Granite 66. -62.4 C-M Nanjing U iversity, 1981 Jiangmukeng, Shao' an, Fujiai Granite 51. C-M Nanjing U iversity, 1981 Shiwatou, Yu xiao, Fujian Admellite 1069 C-M Nanjing U iversity, 1981 Southeast Pin he, Fujian Granite ere aceous C-M Nanjing U iversity,1981 Coastal of Fuj an Alkali Granite ere aceous C-M Lin et aI., 999 Continued

Fonning Thermal IsojOPiC TeIj1perature Pr~ssure Are Rock depth gradient Sources age (Ma) ("C) «(1Pa) (krn) ("C/km)

Dalishan, NOtwest Zhejiang Alkali Granite Early Cretaceous C Zhang et~." 2002 Bashan, North est Zhejiang Alkali Granite 110 C Zhang et ., 2002 Sucun, Suich g, Zhejiang Alkali Granite 86 C-M Wang et aI , 2005 East Zhejiang Tuff 130 86t 0.61 20C 43 Wang, 198 West Zhejiang Tuff in NE trehd 130 100 70 0.6 20C 35 Wang, 198 West Zhejiang Granite in NE ere t100aceous C Yang et al. 1996 Changshan, Z ejiang Rhyolite porp~yry124 C Wu et aI., 984 Chayuan, Zhe iang Rhyolite porp yry 133 C Wu et aI., 984 Jinhua, Zheji g Rhyolite porp yry 133 C Wu et aI., 984 Changle, Che xian, Zhejiang Granite 132 C-M Nanjing U iversity, 1981 Qingjubao,Sh ichang Granite 120 C-M Nanjing U iversity, 1981 Wuxi, Yunhe, hejiang Granite 124~95 C-M Nanjing U iversity,1981 Quanyanton, enzhou Granite 90 C-M Nanjing U iversity, 1981 West Pingyan , Zhejiang Granite 72 C-M Nanjing U iversity, 1981 Qingjie, Ping ang, Zhejiang Granite 76 C-M Nanjing U iversity, 1981 Tangyuankou, Jiangshan, Zhejiang A type granite 124 C Chen et aI. 1991 Qingtian, Zhejiang A type granite 101 C-M Qiu et al., 999 b Putuo, Zhous , Zhejiang A type granite 94 C-M Qiu et al., 999 b Taohua, Putuo Zhejiang A type granite 93 C-M Qiu et al., 999 b Putuo, Zhous , Zhejiang Diorite and alkali gran­ 92-b1.8 C-M Qiu et al., 999 b ite

Taohua ISlandf,coastalOf Zhejiang Alkali granite 90.~3-142.4 C-M Qiu et aI., 1999 b Qingtian, Zhej" ang Alkali granite 1007-114.3 C-M Qiu et al., 999 b Zhejiang-Fuji -Guangdong A type granitelin NE 100 70 C-M Hong et aI. 2002 Liangnong, Yi yao, Zhejiang Granite-syenit 128 103 L Gao et al., 999 porphyry-gabbro Beijie, Shuich g, Zhejiang Alkali granite 86 C-M Wang et aI , 2005 North Changp ,Fujian Granite C-M Nanjing U iversity, 1981 Shao'an, Ch: gpu, Fujian Granite creiceousere aceous C-M Nanjing U iversity, 1981 Yunxiao, Fuji n Granite with arnazonite 100 112 C-M Nanjing U iversity, 1981 Dongshan lsi d, Fujian Granite 66. -62.4 C-M Nanjing U iversity, 1981 Jiangmukeng, Shao' an, Fujiai Granite 51. C-M Nanjing U iversity, 1981 Shiwatou, Yu xiao, Fujian Admellite 1069 C-M Nanjing U iversity, 1981 Southeast Pin he, Fujian Granite ere aceous C-M Nanjing U iversity,1981 {I Coastal of Fuj an Alkali Granite ere aceous C-M Lin et aI., 999 is ~ Continued :ij e£i Forming Thermal >< Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (km) ("CIkm) ~I Zhangzhou Ci y, Fujian 128- 03 C-M Gao et al., 199' .§ Xianglushan, uangze, Fujian rmodal VOlcanj'c 138- 02 C-M Gao et al., 199' Yunshan, Yon tai, Fujian imodal volcanic 138- 02 C-M Gao et al., 199' ~jian i Lingtongshan, Daxi, Pinghe, Imodal volcani c 138- 02 C-M Gao et al., 199' Dayoushan, S ming City, Fu ian 'imodal volcani c 138- 02 C-M Gao et al., 199' ~I Sukeng,Yunxi onanshan, Fuji abbro 65 C-M Gao et al., 199' Xiahebian, Yu xiao, Fujian abbro porphy 70 C-M Gao et al., 199' ~~ Longhai-Shen' 0, Fujian iorite porphyr 77 C-M Ling et al., 19~9 Dayuancun, F jian egirine-augite 95 C-M Wang et al., 2qo5 .ebeckite granite Sukeng, Ping u and Yongcun iabase gabbro 69 C-M Gao et al., 199' Hongshan, Fu hou type granite 99 C Huang et al., 1998 Guizhi, Gush' ,Fuzhou type granite 95 C-M Qiu et al., 1999 b

Wushan, Fuzh u type granite i~NE 95 >8(J( C-M Qiu et al., 200' Jingangshan, outheast Fujian type granite i NE 92 > 8(J( C-M Qiu et al., 200' Xincun, SE Fuiian type granite i NE 92 >8(J( C-M Qiu et al., 200, Shimaoshan, uanshan, Yongtai asalt 113.2 L Qiu et al., 199 a Shimaoshan, uanshan, Yongtai hyolite 106.8 C-M Qiu et al., 199 a Baishiding, Ji ning, Fujian ranite 103 C-M Ling et al., 19 9 Tailaoshan, Fu .ng, Fujian lkali granite 100 C-M Ling et al., 19 9 Yongchun, Fuj an ranite-diorite 120 C-M Ling et al., 19 9 Zhouning, Fuji an ranite 120 C-M Ling et al., 19 9 Zijinshan, Fuji antle inclusion in NW 128-94 800 3.6 86.6L 9 Zhang et al., 21 01 rend Yuanshan, Yoqgtai, Fujian asalt C-M Qiu et al., 199~a Youxi, Fujian yolitic pyroclastic C Wu et al., 198 Yongtai, Fujia C Wu et al., 198 Guanshan, Gu han, Fujian abbro C-M Hong et al., 19 7 Nanyu, Gusha ,Fujian iorite C-M Hong et al., 19 7 Jiantian, Gush n, Fujian rano-diorite C-M Hong et al., 19 7 Danyang, Gus an, Fujian onzonite C-M Hong et al., 19 7 Fuzhou, Gush' , Fujian Ikali granite C-M Hong et al., 19 7 Qianyang, Gu an, Fujian lkali granite C-M Hong et al., 19 7 Guizhi, Gush ,Fujian ranite C-M Hong et al., 19 7 Bijiashan, Gus an, Fujian anitic porphyi C-M Hong et aI., 19 7 Shangfangcun, Zhangzhou roxene diorit. C-M Hong et al., 19 7 Con inued

Forming Thermal Isoto ic Temp rature Press re Are oek depth gradient Scurees age (~a) (9 ) (GP) (km) ("CIkm) Dongjiucun.Zl angzhou, FujiaJ Jiorite 90-H 6 C-M Hong et aI., 19 7 Changtai, Zhm gzhou, Fujian }ranD-diorite 90-[( 6 C-M Hong et aI., 19 7 Gunong, Zhan zhou, Fujian vlonzonitc 90-[( 6 C-M Hong et aI., 19 7 Xineun, Zhang zhou, Fujian J-ranite 90-[( 6 C-M Hong et aI., 19 7 Baishishan, co st of Fujian }ranD-diorite 90-[( 6 C-M Hong et aI., 19 7 Jingangshan, Fujian '\lkali granite Creta eous C-M Hong et aI., 19 7 Xiadashanjia, ongeun, Fujiar 3ranite porphy Creta eous C-M Gao et aI., 199 Huayu, Pengh Islands :Juartz dioritic I orphyry > 61 C-M Gao et al., 199 Huayu, Pengh Islands ndesite > 65 L Gao et al., 199 Western Fujiar Granite in NE Creta eous C Yang et aI., 19 6 Sifang, southw est Fujian J-rano-diorite 104- 08 C-M Mao et aI., 2OC2 Huatuangong, oast ofSE Ch na 3ranite 126 C-M Li WDetal., 998 Jiangmiao, Co st of SE China 3abbro 125 C-M Li WDetal., 998 Zhuanqiao, Co st of SE China rachyte-andesi e 126.6 C-M Li WDetal., 998 Shangfang, Fu ian J-abbro-norite 123 C-M Zhou et aI., 19 4 Changtai, Fujian 3rano-diorite 123 C-M Zhou et aI., 19 4 Yangehunshi, ujian 3rano-diorite 122 C-M Li WDetal., 998 Lingshan.Shan rao, Jiangxi J-ranite 95 C Nanjing Unive sity,1981 Xingzi, Jiujian , N. Jiangxi 3ranite 133, 07 C Nanjing Unive sity, 1981 Yunshan, De'a , Jiangxi 3ranite 114 C Nanjing Unive rsity,1981 South to Guixi Jiangxi 3ranite porphy 90 C Nanjing Unive sity,1981 Shangjia, SE unwu, Jiangxi Jranitoid 114 C Nanjing Unive sity,1981 Northern liangxi 3ranitoid in NE Creta eous C Zhu et al., 200 Wushan, Jiujia g-Ruichang, l' angxi amprophyre n NNE 107 C-M Luo,2006 rend Chengmenshar , Ruichang, Jia gxi ::!uartz keratophyre in 103 C-M Luo,2006 'INE trend Ganjiang, Jiujiang-Ruichang, iangxi 3ranite in NNE trend 100 C-M Luo,2006 Chengmengshi n, liujiang ::!uartz porphyrj Creta eous C-M Jiangxi Geolog ieal Survey, 19 3 Guangfeng-Sh ngrao, Jiangxi Iholeiite E. Cr taceous 56 Liao et aI., 1999 Guangfeng-Sh ngrao, Jiangxi lkali basalt L.Cre aceous 83 Liao et al., 1999 Southern Jiang i Kimberlite cor glomer- Creta eous L Lai et aI., I99~ te Northeastern J angxi ntennediate-ae d E. Cr taceous C-M Wang et aI., 2000 Jiangshan, Zhe .iang-Guangfeng, Jiangxi holeiite, Atkal basalt 98-[(5 C-M Yu et aI., 2004 {I Jiazi, Lufeng , Guangdong J-ranite 99-[( 0-126 C-M Nanjing Unive rsity,1981 is ~ Con inued :ij £i Forming Thermal e Isoto ic Temp rature Press re >< Are ock depth gradient Scurces age (~a) (9 ) (GP) (km) ("CIkm) ~I Shan wei, sout Haifeng,Guan dong 3ranite 112 C-M Nanjing Unive rsity,1981 .§ Qiniangtan, N' TVHuiyang,Guangdong 3ranite 136- 32 C-M Nanjing Unive rsity,1981 North Boluo, ( uangdong J-ranite 91-1 7 C-M Nanjing Unive rsity,1981 i Kunshan, Zen, cheng, Guangd ng J-ranite 132 C-M Nanjing Unive sity,1981 Tangkou, Yangchun, Guangdo g 3ranite 119 C-M Nanjing Unive rsity,1981 ~I Liantang,Chen ai, Guangdong J-ranite 90 C-M Nanjing Unive rsity,1981 Tangkou, Dian ai, Guangdong J-ranite 108 C-M Nanjing Unive sity,1981 ~~ Southeast Ziji , Guangdong 3ranite 100 C-M Nanjing Unive rsity, 1981 NE Yangchun, Guangdong 3ranite 125 C-M Nanjing Unive rsity,1981 Huangtian. He ai, Guangdong lkali granite 84.8 C-M Cui, 1989 Yingqiao, Lian iiang, Guangdo g 3ranite Creta eous C-M Wang et al., 1999 East Guangdo g 3ranitoid Creta eous C Yang et al., 19 6 Naqing, South Anping, Guang ong Jranite 130- 36 C Nanjing Unive sity,1981 Yangchun, we t Guangdong J-ranite diorite 125 C-M Geng et al., 20 6 WesternGuan dong 3ranite diorite , Mon- 100 C Geng et al., 20 6 onite Rhyolite acite Xinpeng, West rnGuangdong Jranite 116 C Wang et al., 2003 Yingwuling, " estern Guangd ng J-ranite 67 C Wang et al., 2003 Xishan, Weste n Guangdong Jranite 81 C Wang et al., 2003 Xiaonanshan, Nestem Guang ong 3ranite 55-8 C Wang et al., 2003 Yinyan, Weste n Guangdong 3ranite 80.5- 2.3 C Wang et al., 2003 Xiping, Weste n Guangdong Jranite 81-1 9 C Wang et al., 2003 Shilu, Western Guangdong 3ranite 122 C-M Wang et al., 2003 Tangpeng, We tern Guangdon 3ranite 132 777.7 0.848 32 24 Wang et al., 2003 Tongzigen, Western Guangdor g Jranite 98 C-M Wang et al., 2003 Baiyunzhang, ast Guangdon '\clkalirhyolite, achyte 140- 29 C Zhang, 2001 Liangkou, Con ghua, Guangdo g yenite 137-i 6 C-M Wang et al., 2005 Qilin, Shantou Guangdong 3ranulite in BIDalt 112 C-M Xu et al., 1999 Huichang, Jian gxi, Rencha,Guangdong Basaltic dyke 93-1 9 L Zhang et al., 2 04 Zhuguangshan and Guidong.C uangdong cid rock dyke 85.9- 2.7 C-M Zhang et al., 2 04 Yaji, Fogang, ( uangdong Ikali rock 127 C-M Li et al., 1998 Longmenshan, Emanzhen, Ha nan asic-acid bim dal vol- 138- 02 L Gao et al., 199 anie Dachang, Nan an, Guangxi 3ranite 91 C Nanjing Unive sity,1981 Kunlunguan, SE Pinyang, Gus ngxi 3ranite 108- 29 C Nanjing Unive rsity, 1981 Darning, Soutf Mashang, Gua gxi J-ranite 86-8i C Nanjing Unive rsity,1981 Contmued Forming Thermal Isotopic Temperature Pressure depth gradient Sources Area Rock age (Ma) ("C) (GPa) (Ian) ("CIkm) Huarong, Hunan Granite 110 C-M Nanjing University, 1981 Tianjingshan, East Huarong, Hunan Granite 119-127 C-M Nanjing University, 1981 Northeast Pingjiang, Hunan Granite 110 C Nanjing University, 1981 South Mufushan, Hunan and Hubei Granite 127-100 C Nanjing University, 1981 Wangxiang, Changsha, Hunan Granite 127 C Nanjing University, 1981 Tongshanling,Jiangyong, Hunan Granite 91-110 C Nanjing University, 1981 Shuikoushan, Changning, Hunan Granite 106 C Nanjing University, 1981 Baimashan, East Qianyang, Hunan Granite 107 C Nanjing University, 1981 Northwest Xitian, Hunan Granite 128-130 C Nanjing University, 1981 Ningyuan-Daoxian-Shiwandashan Basalt in NE trend 132-135 1,083 2.2 70--85 14 Zhu et a!., 2005 Rucheng, Southeast Hunan Diabase, basalt 112-128 C-M Jia, 2003 Northeast Hunan Basalt 85-95 L Xu et a!., 2006 Yingjiashan, Northeast Hubei Alkali Basalt 62.1 L Peng et aI., 2006 Tiantangzhai Dabieshan Granitoid 131 830 0.54 18 46 Wang et a!., 2000 Jiutai, Jilin Dacite Cretaceous 1,276 1.27 42M 30.4 Lu et aI., 1996 Jiutai, Jilin Dacite Cretaceous 70--80 Lu et aI., 1996 East Zhejiang Tuff 130--100 866 0.6 20 43 Wang, 1986 West Zhejiang Tuff 130--100 707 0.6 20 35 Wang, 1986 West Zhejiang Granitoid Cretaceous <22 Yang et a!., 1996 West Fujian Granitoid Cretaceous <25 Yang et a!., 1996 Zijinshan, Fujian Granitoid 128-94 800 2.6 86.6 9.2 Zhang et a!., 2001 East Guangdong Granitoid Cretaceous 75 Yang et a!., 1996 Fuxin, Liaoning Peridotite 84.8 1272 2.93 97.7 18.4 Zheng,1999

North Sinian Period 56-23 Ma Fushun, Liaoning coal metamorph. Paleogene 29 Yang et a!., 1996 Hannuoba, Hebei Granulite Paleogene 900 1.1 36.7 24.5 Chen et a!., 1998 West Tengchong Granulite 27-17 720 0.8 26.7 27 Ji et al., 1998 Labieshan, Yunnan Anphibolite 23.1 720 0.8 26.7 27 Ji et al., 1998 South east Xizang Eclogite 49 650 2.6 86.7 7.5 Zheng et a!., 2001 Beibuwan Sandstone-shale Eocene TL 36.7 Wang et a!., 1995 Beibuwan Sandstone-shale Oligocene TL 34.6 Wang et a!., 1995 Zhujiang-Sanshui Sandstone-shale Eocene TL 39.4 Wang et al., 1995 ~I Beibuwan Sandstone-shale Oligocene TL 38.9 Wang et al., 1995 '0 Yinggehai basin Sandstone-shale Oligocene TL 43.7 Wang et a!., 1995 "0 "is ~ Continued :ij e£i Forming Thermal >< Isotopic Temperature Press~re Are Rock depth gradient Sources age (*a) (t) (GP4) (Ian) ("CIkm) ~I West Qaidam andstone-shal Eocene reflectivity of 24 Zhou et al., 1998 .§ coal Liaohe basin andstone-shal Eoce e 45 Zhou et al., 1998 i Liaohe basin andstone-shal Paleo ene FT 42.3 Zhou et al., 1998 Xihu basin, Donghai andstone-shal 40-2 Ff 28 Jiang et aI., 2001 ~I Dongying basip andstone-shal Paleo ene 48.2 Zeng et al., 2000 Tarim basin andstone-shal Paleo ene 26-20 Pan et aI., 1996 ~~ Shi wandashan Sandstone-shal Paleo ene ~21 Wang, 1998 North Jiangsu andstone-shal Paleo ene ~30 Wang et al., 1989 Liaohe basin andstone-shal Paleo ene ~34 Wang et al., 1989 Bohaiwan andstone-shal Paleo ene ~36 Wang et al., 1989 Yitong VOlcalnc area, Jilin 'holeiite 31 M Zhang et aI., 2006

Hengshantou, itong lkaliolivine btSalt 31 L Liu et al., 1992 Sifangtingzi, uinan, Jilin Ikali olivine b salt 27.3 L Liu et al., 1992 Malugou, Dun ua, Jilin ~Ikali olivine b salt 27.9 L Liu et al., 1992 Yongshen, So th Jilin yenite 31 L Yuan et al., 2003 Huanghua, M danjiang, Heilongjiang 44.9 L Liu et al., 1992 Chifeng, Inner Mongolia Q~~~iteand !OliVine 33-2 L Jia et al., 2002 lholeiite lining, Inner Mongolia 'holeiite, olivi basalt, 33 M Zhang et al., 2005, 2006 asanite, alkali asalt Panjing, Liaon ng )\lkali olivine b salt 24.8-$1.4 L Liu et al., 1992 Yingmawan, E stem Liaoning Gabbro 32 L Yuan et aI., 2003 Oulituozi, Lia he Basin rachyte 38-4 L Zhang et al., 2006 Dongying Fo ation, Lower LJaohe Depres­ Oligocene L Compiling Group of Petrol. Geol., 'holeiite, pYro~ne SIOn asalt 1993 Fangshenpao, ower Liaohe epression Ikali olivine b salt L OligO~ene Lower Liaohe epression asalt in NNE end 35.9- 6 M Liu et al., 1992 Shuiquanzhen, Weixian, Hebe: lkali olivine b salt 29.3 L Liu et al., 1992 Hannuoba, He ei anulite in bas t Eoge e 900 1.1 36.7 C Chen et al., 1998

Yangyuan, He ei ridtieand yroxen- o t29.3- 2.2 L Ma et al., 2006 te in basalt Shayiduan, Huanghua, Hebei ~iabase Oligocene L Compile Group of Petrol. Geol., 1993 Sha' erduan, Huanghua, Hebei Basalt Oligocene L Compile Group of Petrol. Geol., 1993 Shayiduan-Shasanduan, North' Huanghua pabbro and Diabase Oligocene L Compile Group of Petrol. Geol., 1993 Continued

Forming Thermal Isotopic Temperature Press4re Are ock depth gradient Sources age (l\fI.a) ('¢) (GP~) (km) ("CIkm) Shayiduan, Huanghua Diabase Oligocene L Compile Grou of Petrol. Geor' 1993 Dongying Formation, Qikou, JlIanpu, Diabase in NE trend Uppe L Compile Gro p of Petrol. eol., Oligocene 1993 Western Qikou-Nanpu holeiite, in NNE trend Uppe L Compile Gro p of Petrol. eol.,

OligO~ene 1993 Shayiduan, z~nhua,Shenli asalt Eoge e L Compile Grou of Petrol. Geo ., 1993 Shasanduan, iming livine Basalt Eoge e L Compile Grou of Petrol. Geo ., 1993 Dongtai, Wuta shan, Shanxi [ iabase 51.9 L Shao et al., 20 5a Shuiyao, Zuoy n, Shanxi Ikali olivine basalt 47.5 L Shao et al., 20 5a Fanshi, Shanxi holeiite, Alkali olivine 26-31 L Liu et al., 1992 asall Yingxian, Shii imberlite Eogerie A Dong,1994 Nvshan, Anhu asalt in NNE Jend 36-5. M E and Zhao, 19~7 Tuanshanbao, uangde, Anhu asalt 42.6 L E and Zhao, 19~7 Northern Jiang u Basin holeiite, Alkal olivine 46-651 L Liu et al., 1992 asalt Nanhui, Shang ai Ikali olivine b salt 26.7 L Liu et al., 1992 Gaoyou, Jiang u Ikali olivine b salt 46.3 L Liu et al., 1992 Northern Jiang u Basin holeiite L EOgeJe E and Zhao, 19!7 Jintan Basin, J angsu oleiite Eoge e L E and Zhao, 19 7 Zhaomingshan Anhui holeiite Eoge e L E and Zhao, 19 7 Wuyuanshan, nhui holeiite Eoge e L E and Zhao, 19 7 Tuanshan, Gu gde, Anhui livine tholeiit. 42.6 40-50 Wu et ai, 1984 Balinshan, Ji glin, Hubei oleiite 52 L Liu et al., 1992 Baishe, Nanfe g, Jiangxi afiC-Ultramafit rocks 37 L Gao et al., 199 Southeastern oastal Area holeiite 50 L Li et aI., 1998 Sanshui-Heyu -Lianping, Guangdong livine basalt .n E-W 61-451 L Zhu et al., 200 rend Leizhou,panin~ula,Guangdon livine basalt ij E-W 5 1,100+1,200 1.5-2.10 77 16 Zhu et al., 200 61-4 1 Mashan, Guan xi livine basalt i E-W 61-45 L Zhu et al., 200 Maguan, Yunn n livine basalt i E-W 61-45 1,337 4.1-4.17 >60 22 Zhu et aI., 200

Hamalayan Period 23-0. 78 ~a Yarlung Zangbo ~Iancophane <23 350 0.8--0·196 26.7-32 ~1O Xizang Geological {I Nyalum, Xizang nphibolite <20 650 0.72 24 ~24 Survey, 1993 is ~ Continued :ij e£i Forming Thermal >< Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (ON) (km) ("CIkm) ~I Yadong, XiZ nphibolite <20 670 0.8 28.5 ~23 Survey, 1993 .§ Gamba, Xizan nphibolite 21-1 560 0.7 23.3 ~24 Survey, 1993 Southeast Xiz g ranulite 17-1 850 1.8 60 ~ 17 Zhai,1998 i Dabieshan ylonite Neog ne 350 0.6 20 17.5 Liu et aI., 199( Central mount ins of Taiwan een schist Mioe ne 300 0.4 13.3 22-23 ~I Chen et aI., 1914 Yuli, Taiwan1 reen schist L. Mi cene 350 0.6 20 17-18 Chen et aI., 19 4 Tailuge, Taiwa reen schist 35-2. 6 475 0.5 16.7 28-29 Chen et aI., 19 4 ~~ North Nanhai patite >10 FT 34 Deng et aI., 19 7 Leizhou, ouan~dong ranulite Ceno oie 1,160 1.7 56.7 27 Yu et al., 1998 Beibuwan andstone-shale Neog ne TL 31.1 Wang et al, 19 5 Zhujiang-Sans ui andstone-shale Neog ne TL 37.2 Wang et al, 19 5 Yinggehai bas" andstone-shalc Neog ne TL 38.7 Wang et al, 19 5 Kalpin, Xinjia g andstone-shale Neog ne 7~21.3 Wei et aI., 198 Tarim basin andstone-shale Neog ne reflectivity of 20 Fan et aI., 199 coal Erdos basin andstone-shale 28 Ren et aI., 199 NeOgjne Keluo, Nengh~Heilongjiang 'eridotite inclusion 5.4-25 1,100 2.6 85.6 13 Chi et aI., 198 Ludao, Heilon [iang erzolite Neog ne L E and Zhao, I ~87 Shangzhi,Yua bao, Heilongjiang erzolite Neog ne L Chi et aI., 198 Jingpohu-Beih tou Heilongjiang ~erzolite, dunite Neog ne L E and Zhao, 1 87 arzburgite L E and Zhao, I Q87 Jingpohu, HeJ'1ngjiang NeOgjne Mudanfeng, udanjiangshi Neog ne L E and Zhao, 1987 erzolite,dnnit Kedong, Heilo gjiang erzolite, duni Neog ne L Liu, 1983 Wudalianchi, eilongjiang pinel Iherzolit Neog ne L Qiu et aI., 199 Shangzhi, Hei ngjiang lkali basalt in NE 18.9- 7.7 1,412 2.2 73 19 Liu et al., 199 Nengjiangxian Heilongjiang ~lkali olivine b salt 2.5 L Compiling Group of Petrol. IOeol., 1993

ShifenggOU,~ng,anxian asalt 6.35 L Ning'anxian, eilongjiang lkali olivine basalt 7.59 L Wuchagou, Ding Oil field asalt L Daluorni, Daqi g Oil field asalt NeogNeog§ene Jidong-Dongni g, Daqing asalt Neog ne Huanghua, Da ing Oil field asalt Neog ne Donghua Fo ation, Daqing asalt E.Qu . Jingpohu, Heil ngjiang asalt E. Qu . Continued Forming Thermal Isotopic Temperature Pressure depth gradient Area Rock age (Ma) ('C) (GPa) Sources (km) ('CIkm) Wangtianhe, Changbaishan, Jilin Trachyte basalt, andesite 2.12-2.87 M Fan et aI., 1998 Jingyu, Jilin Peridotite inclusion in 15-1.48 1,450 2.8 91.8 16 Chi et aI., 1988 NNE trend Wangqing, Jilin 6.2-2.1 1,320 1.9 62.5 21 Chi et al., 1988 Wangqing, Jilin 6.3-2.1 880-1,100 1.4-2.3 52-70 17-16 Wang et aI., 2000 Yitong, Jilin 21-7.8 1,410 2 67 21 Chi et al., 1988 Huinan, Jilin 15-1.48 1,252 2.1 71 18 Chi et al., 1988 Changbaishan, Jilin 6.4-3.1 1,460 2.5 85 17 Chi et aI., 1988 Da-Xiaogusha, Ma'anshan,Yitong lherzolite, and pyroxe- Neogene L Wu,1984 nite Spinel Jiaohe, Jilin Neogene L Wu,1984 Erdaobaihe, Antu, Jilin lherzolite Neogene L Liu,1983 Dayishan, Huinan, Jilin lherzolite, harzburgite, Neogene L Luo,1984 dunite, websterite Dalongwan, Huinan, Jilin Neogene L Wu,1984 Laomiao, Jilin lherzolite inclusion Neogene L E and Zhao, 1987 Qixingshan, Shuangliao, Jilin lherzolite, pyroxenite Neogene L E and Zhao, 1987 Houtuanshan, Yongji, Jilin Peridotite Neogene L Chi et al., 1988 Fengmang, Jilin Basalt, Alkali olivine 4.9-5.3 L Liu et aI., 1992 basalt Houtuanshan, Jilinshi, Jilin 13.2-22.3 L Compiling Group of Petrol. Geol., 1993 Wangqing, Jilin Basalt 2.13 L Compiling Group of Petrol. Geol., 191 Dunhua, Jilin Alkali olivine basalt 23.9 L Compiling Group of Petrol. Geol., 19 Dagushan, Yitong, Jilin Basalt 12.8 L Compiling Group of Petrol. Geol., 1993 Xiaogushan, Yitong, Jilin Basalt 10.4 L Compiling Group of Petrol. Geol., 191 Dongjianshan, Yitong, Jilin Basalt 9.74 L Compiling Group of Petrol. Geol., 19 Sulan, Jilin Alkali olivine basalt 12.4 L Compiling Group of Petrol. Geol., 1993 Yongjixian, Jilin Basalt Miocene L Compiling Group of Petrol. Geol., 191 Chandishan, Huadian, Jilin Basalt Miocene L Compiling Group of Petrol. Geol., 1993 Junjianshan, Helong, Jilin Basalt 13.5-28.4 L Compiling Group of Petrol. Geol., 19~~~I Wangqing, Jilin Basalt Neogene 1,310-1,330 1.5-2.2 53-70 23-19 Liu et al., 1992 '0 Tianchi, Changbaishan, Jilin Trachyte-basalt 2-D.1 L Fan et al., 2006 "0 "is ~ Continued :ij e£i Forming Thermal >< Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) C'(:) (GN) (krn) ("CIkm) ~I .§ Yitong, Jilin asalt 9-15 A Zhang et al., 2~06 Malianshan, Qingyuan, Liaoning lkali olivine basalt 5.5-7 L E and Zhao, 1 87 Guantao, Xialikohe tasalt Neogene L Compiling Gr up of Petrol. IGeol., i 1993 L ~I East basin, Xix.iaohe saltin NE trId MiOC!ne Fuxian, Liaoni g logite in NN trend Neog ne 1,150 2.5 83.3 L Zhou,1996 Kuandian, Lia ning livine tholeiit , Alkali Neog ne 1,3901-1,430 1.8-215 60-80 23-18 Lu et al., 1981 ~~ livine basalt g ebsterite Neogene 1,675 4.35 143 12 Lu et al., 1981 Kuandian, Lialin Huangyishan, uandian, Liaoning arzburgite, websterite Neogene L Lu et al., 1981 Huashan, She ang, Liaoning ~lkali olivine bhsalt 9.76 L Liu et al., 199 Qingyishan, K andian, Liaoning herzolite L Liu et al., 198 Neogine Liujia, Kuandi n, Liaoning herzolite Neog ne L Liu et al., 198 Zhen'an, Beining, Liaoning 'eridotite Neog ne L Chi et al., 198 Longgang, Lia ning pinel iherzoli e web­ Neog ne L Yang et al., 19~4

~terite Dayishan, KUfdian, Liaoning f\lkali olivine b salt 1,1291-1,330 1.7-211 55-70 21-19 Luo,1984 Northeast Chi a 'eridotite in N E trend NeogNeogjnene 1,118 2.76 80-91 14-12 Qiu et al., 199 Hexigtun, Inn Mongolia hoshonite 0.89- .74 L Liu et al., 199 Xilingol, Inne Mongolia 'eridotite in E trend 15.6- .9 1,450 2.2 73.3 20 Chi et al., 198 Siziwang, Inn Mongolia pinel Iherzolit Mioe ne 1,1001-1,250 1.7-210 77 14-16 Chen et al., 201M Sanyitang, Jini g, Inner Mongolia 'yroxene maer -crystal Neog ne 950 1.5 50-60 19-16 Du et al., 2005 n Spinel iherzo ite lining, Inner ~ngOlia ontinental flo d basalt Mioc:ne L Liu et al., 199 Zuoyun, Inner ongolia ontinental flo d basalt Mioe ne L Liu et al., 199 Weichang, Inn r Mongolia ontinental flo d basalt Mioe ne L Liu et al., 199 Chifeng, Inner Mongolia asalt 10-6 L Jia et al., 2002 South to Xann ron River asalt 4.8 L Jia et al., 2002 Hexigten, Inne Mongolia asalt 0.89 L Jia et al., 2002 lining, Inner ongolia oleiite, OliVitbasalt, 22.8- 2.1, M Zhang et al., 2$05, 2006 asanite 12.2- .4 Arxan, Inner ~ongOlia antle source i elusion Neogl·16ne L Yu et al., 2006 Abag Qi, Inne Mongolia lkali olivine b salt 5.44 L Liu et al., 199 Fengzhen, Inn r Mongolia oleiite 8.84 L Liu et al., 199 Dawang, Feng hen, Inner Mongolia 'holeiite 7.48 L Liu et al., 199 Hanuoba, Heb i 'eridotite in NNE trend Neogene 1,110 2.16 70 16 Li et al., 1999 CIS' --.l Continued 0 Forming Thermal Isotopic Temperature Pressure depth gradient Area Rock age (Ma) ('C) (GPa) Sources (krn) ('CIkm) Hanuoba, Hebei Granulite inclusion Neogene 800-950 1.11 43 19-22 Chen et al., 1998 Zhangjiakou, Hebei Continental flood basalt Miocene L Lin et al., 1992 Darnaping, Hebei Peridotite in NNE trend 24.3-3.9 1,380 3.2 105 13 Chi et al. 1988 Pingquan, Hebei 24.5 1,400 2.3 76.4 18 Chongli, Hebei Garnet lherzolite in Neogene Liu et al., 1985 basalt Shexian, Hebei Eclogite in kimberite Neogene 1.0 L Dong, 1994 Shizijie, Zhangbei, Hebei Tholeiite 13.7 L Lin et al., 1992 Zhangbei, Hebei Alkali olivine basalt 17.8 L Lin et al., 1992 Darnaping, Wanquan, Hebei Basanite 21 L Liu et al., 1992 Wuluogongshan, Weichang, Hebei Alkali olivine basalt 26 L Liu et al., 1992 Qipanshan, Weichang, Hebei Alkali olivine basalt 7.26 L Liu et al., 1992 Zhouba, Zhangbei, Hebei Tholeiite 22.8 L Liu et al., 1992 Xiaosuangou, Shangyi, Hebei Tholeiite 4.38 L Liu et al., 1992 Luotuofeng, Pingquan, Hebei Tholeiite 24.3 L Lin et al., 1992 Yangyuan, Hebei Peridotite in basalt Neogene 975-1,054 1.1-2.2 35-68 28-16 Liu et al., 2006 Baigezhuang, Beijing Tholeiite 15.9 L Liu et al., 1992 Baicaoping, Wu'an. Hebei Olivine basalt 3.52-4.3 L Liu et al., 1992 Jingxing, Hebei Alkali olivine basalt 6.31 L Liu et al., 1992 Center-North Dagang Oil Field Basalt in NNE trend Miocene L Compiling Group of Petrol. Geol., 1991 Gangdong, Dagang Oil Field Basalt Pliocene L Compiling Group of Petrol. Geol., 19~~ Qikou, Well Qinan I, Dagang Oil Field Basalt Pliocene L Compiling Group of Petrol. Geol., 19 Gaoshangbao, Dagang Oil Field Olivine basalt 22.1 L Liu et al., 1992 Huangjiawa-Datong Shanxi Spinel lherzolite E.Quart. 900-1,050 1.1-1.7 40-60 23-18 Chen et al., 1997 Dongtaigou, Wutaishan, Shanxi Spinel lherzolite Neogene L He et al., 1983 Fenghuangshan, Xiyang, Shanxi Alkali olivine basalt 7.25 L Liu et al., 1992 Jiaoyanshan, Linju, Shandong Alkali olivine basalt 14.3-20.7 L Liu et al., 1992 Xiaoshanwan, Linju, Shandong Alkali olivine basalt 13.2-14.2 L Lin et al., 1992 Dafangshan, Qixia, Shandong Olivine nephelinite 8.13 L Lin et al., 1992 Daheishan Island, Penglai Alkali olivine basalt 8.08 L Lin et al., 1992 Fushan, Pingdu, Shandong Basanite 7.99 L Liu et al., 1992 Linju, Shandong Monoclinic in basalt 4-14 L Zhang et al., 2006 ;J> Qijiadian, Shan dong Peridotite inclusion in Neogene 875 4.1 136 7 You, 1998 "" ""e NNE trend '"0. is' .a Continued ~ £i &. Forming ThennaJ x Isotopic Temperature Press~re Are ock depth gradient Sources -..J age (*a) C'(:) (GN) (km) ("CIkm) (;l .g Shanwan-Charigle, Shan dong pinel IherZOlitj pyrox- Neogene L Zhao et aJ., 19$2 nite Qixia-Penglai.lghandong herzolite, spin I Neogene L Zhao et aJ., 19J2; ,I arzburgite, pyr xenite, Liu et aI., 198 ; iaJlage-peridot te Zhang, 1982; in, 1982 ~ LinJ~' lkaJi olivine b saJt 50-80 Wu et aJ., 198 Shanwan, Shandong NeogEe Huashan-Daxi o-Fangshan, Q xia herzolite inclu ion EQu . L Wu et aI., 198 ~~ u Chishan-Xish , Penglai asanite, phon ite Neog ne L Wu et aJ., 198 .g Guantao Form lion, Huiming ~hengliField livine basaJt Neog ne L Compiling Grtup of Petrol. IGeol., 9­ i 1993 § Shangyu, HebiL Henan pinel lherzolite, Spinel E.QuF· L Yang et aJ., 19 6 0- arzburgite Liu et aI., 198 ;l

Hebi, Henan imberite E.QU~. A Dong,1994 ~ Pangeun, Heb · Henan lkaJi olivine b saJt 4.32 L Liu et aJ., 199 ~ Heishantou, P geun, Henan ~Ikali OliVineJSaJt 3.99 L Liu et aI., 199 Da'ancun, Rutaang, Henan .holeiite 6.83 L Liu et aI., 199 ~ Liuhe, Jiangsu 'eridotite in E trend 1,193 1.5 50 24 Zhi et aJ., 199( Neogine g Liuhe, Jiangsu Plioe ne 1,052 2.06 68.7 15 Dong et aI., 5' Liuhe, Jiangsu 16.3- .6 2.2 74 14 Sun et aJ., 199113 Liuhe, Jiangsu 16.3- .6 1.2- 116 46-52 19 Wang et aJ., 2 0 ,.,.~ ~o~~~182 NaJianshan, Liuhe, Jiangsu pinel Iherzolin 4 1,032 1,080 1.7-19 56-63 17 Chen et aJ, 19 4; Zhi et al, 2001 ~ Fangshan, Li~e,Jiangsu pinel Iherzolit 1,08 1,178 6 75-85 14 E and Zhao, 1 87 Neo~ne 2.3-2r: 5' Guafushan, Li he, Jiangsu pinel Iherzolin Neog ne 1,113 1,237 2.25- .2 74-100 15-12 E and Zhao, I 87 (jq en Fushan, Liuhe, Jiangsu pinel Iherzolit Neog ne 1,13 1,216 2.5-32 80-100 14-12 E and Zhao, I 87 Pingmingshan, Donghai Jiangsu 4.02 .38 830- 00 1.5-17 56-65 15-14 Zhao, 1982 pinel IherzOli~' ~ arzburgite, we sterite Jin et aJ., 2003 g., Nvshan, Mingguan, Anhui 'eridotite in N E trend E.Qu.\rt. 1,100 1.9 63.3 17 Jin et aJ., 1998 ne- Nvshan, Mingguan, Anhui pinel iherzolit , spinel 16.5-1.4 1,029 1.9 62 17 Sun et aJ., 199, 5' cc Iivine websteri e n 5.4 900-1,128 2 0 38--<>5 24-17 c Nvshan, Mingtan, Anhui 16.5-1 1.1- 1 Wang et aI., 2iO g Dangtu.Anhui 16.5- .4 1,174 2.9 92 13 Sun et aJ., 199 5' Jingong, Huai ing, Anhui Neog ne L E and Zhao, I 87 g Xishanqiao, N njing f'.lkali olivine I basalt, Plioe ne 40-80 Liu et aI., 199 Iivine tholeiite Yaomai, Nanjing Pliocene 40-80 Liu et aI., 199 :"J ~ Continued tv

Forming Thermal Isotopic Temperature Press~re Are ock depth gradient Sources age (*a) (GN) (t) (km) ("CIkm) Chishan, Juro , Nanjing Pliocene 40-80 Liu et aI., 199 Pingmingshan, Donghai, Jiangsu 6.10 L Liu et aI., 199 Guafushan, Li he, Jiangsu 9.35 L E and Zhao, 1 ~~:~::livin teb!Salt Fangshan, Liu e, Jiangsu Ikali olivine b salt 8.60 L E and Zhao, I Chishan, Juro , Jiangsu livine basalt 13.9 L E and Zhao, 1 Liyang, Jiangs lkali olivine b salt 20.7 L E and Zhao, 1 Shangxing, Li ang, Jiangsu Ikali olivine b salt 15 L E and Zhao, I Chuansha, Sha ghai ilkali olivine b salt 18.7 L E and Zhao, 1 North Jiangsu asin holciite 9.18 L E and Zhao, I Tushan, Anhui pinel iherzolit 10 1'168 5.2 82 14 E and Zhao, I Neogjne 1' Dashushan, H fei, Anhui Neog ne 1,1181 1,159 2.9 90 13 E and Zhao, 1 Xinchang, Zh [iang herzolite in NNE Neog ne 1,210 2.4 80 15 Lin et aI., 199 Xinchang, Zhejiang Basalt Neog ne 1,46 1,500 2.0-215 96 16 Zhao, 1990 Xilong, Quxia , Zhejiang pinel Iherzolit Neog ne L E and Zhao, 1987 arzburgite Quxian, Zhejiang Nephelinite I Neogene 1,540 2.9 80.5 19 Zhao, 1990 Jinyun, Zhejiang :pinel Iherzolite pyrox- Neogene L E and Zhao, 1987 nite Zhongfu, LoniOU, Zhejiang 'eridotite Neo g L E and Zhao, 1~87 Talong, Longy u, Zhejiang 'eridotite Neog ne L E and Zhao, 1 87 Huangyan, Zh jiang pinel Iherzolin Neog1nene L E and Zhao, 1 87 Xinchang-Tia tai, Zhejiang holeiite, Alkaj olivine 6-7 L Liu et aI., 199 asalt Mingxi, Fujiar 'eridotite in N E trend Neog ne 1,115 1.84-r,.6 59-79 16 Peng et al., 19'i10 Mingxi, Fujiar asanite Neog ne 1,49Of-1,510 2.5 112 14 Zhao, 1990 Mingxi, Fujiar ephelinite Neog ne 1,515f-1,550 2.7-29 108 14 Zhao, 1990 Mingxi, Fujiar asalt Neog ne 1,500 3.5 135 11 Zhao, 1990 Xilong, Fujian amet Iherzolit Neog ne L E and Zhao, 1'187 Longhai, Fujia i'eridotite in NNEtrend Neog ne 1,016 1.7 56 18 Peng et al., 19~0 Minqing, FUjit Neog ne 1,270 3.7-415 130 10 Xu et al., 1995 Minqing, Fuji Neog ne 1,4001-1,430 1.5-20 77 19 Zhao, 1990 Niutoushan, S ouning, Fujian pinel lherzolite in AI­ Neog ne L Yue et aI, 20051 ali basalt Niutoushan, Shouning, Fujian Basalt Neogene 1,350 1.2-116 61 22 Zhao, 1990 Dayang, Mingxi, Fujian Gamet spinel lherzolite, Neogene L Sun and Lai, 1980 arzburgite i0. is' .a -;J> '0 Continued (1) "&. Forming Thennal x Isotopic Temperature Pressure -..J depth gradient Area Rock age (Ma) ("C) (GPa) Sources (;l (km) ("CIkm) '0a Shiheng, Mingxi, Fujian Spinel lherzolite dunite Neogene L Sun and Lai, 1980 (1) ~ harburgite @ Mingxi, Fujian tholeiite, Alkali basalt, 0.1-25.1 L Gao et aI., 1999 andesite '" ~ Minqing, Fujian 0.1-25.1 L Gao et aI., 1999 ~ Changpu, Fujian 0.1-25.1 L Gao et al., 1999 u Liuhui, Longhai, Fujian Tholeiite 17.6-18.1 L Liu et al., 1992 .g 9- Xiangshan, Longhai, Fujian Tholeiite 17.5-17.7 L Liu et aI., 1992 cc Niutoushan, Longhai, Fujian Tholeiite, Alkali olivine 11.7-16.7 L Zhou, 1981 0- "-3 basalt e- (1) Penghu Islands Basalt, in NNE trend 2 L Chen, 1973 a Penghu Islands Tholeiite, Alkali basalt 16.2-8.2 C-M Liu,1999 ~ Penghu Islands Tholeiite, Alkali basalt, 0.8-25.1 L Gao et aI., 1999 o OJ &. andesite (1) Taiwan 0.8-25.1 L Gao et aI., 1999 g a' Pengjiayu, North Taiwan Andesite, basalt 3.6-1.6 L Liu,1999 ~ 0 Datun volcano, North Taiwan Andesite, basalt 2.8-0.8 C-M Liu, 1999 ,.,. Jilong volcano, North Taiwan Andesite, basalt 1.7-0.81 C-M Liu, 1999 "

Lanyu, Southeast Taiwan Andesite 13.5-2 L Liu, 1999 ~ a' East Taiwan longitude valley Basalt in NNE trend 25-1.85 L E and Zhao, 1987 (jq Puning, Shantou, Guangdong Peridotite in NNE trend Neogene 1,380 1.7 55.5 25 Chi et aI., 1988 en Puning, Shantou, Guangdong Alkali basalt Neogene 1,300-1,380 1.4--1.65 46 28 Zhao, 1990 (jq'" Puning, Shantou, Guangdong Pyroxenite Neogene 1,490-1,570 2.2-2.7 100 15 Zhao, 1990 ~ -.,0 Coast of Fujian and Guangdong Pyroxenite in NE trend 20-1.8 1,050 1.7-2.3 50-80 21-13 E and Zhao, 1987 n Tianyang-Yingfeng, Xuwen, Guangdong Spinel lherzolite, Neogene L Hu and Zhong, 1982 e- a'cc harzburgite, Pyroxenite n 0 Wenchang-Anding, Hainan Neogene L Hu and Zhong, 1982 g

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~OOE Ridge,231 B back-arc basin hypothesis,2991 a ttc ate, Banggongco-NujiangCollisionBelt, 210 -type, 186,205 Banggongco-Nujiang CollisionZone, 197 -type alkali granite,206 Bangong-Nujiangand Yarlung Zangbo RiverCretaceous ba-Garze-Litang region, 135 PaleogeneCollisionBelt, 2 abyssalfacies, 185 Baoshan-SibumasuBlock, 165 accretioncomplex,230 basalt, 251, 259 ccumulationof hydrocarbons and mineralresources, 205 basalticdyke, 205 ccumulationof mineraldeposits,351 base of the lithosphere,205, 209 ccumulationof oil and gas, 185, 348, 356 basementfault, 350 · ccumulationof petroleum,227, 230 basic dyke swarm,55, 248 · ctivationof platforms,291 basin and range tectonics, 197 · ctive(or "catastrophic")period, 3 basin-and-range structure,203 · ggregationof planetesimals, 27 basins,205, 228 alkali-basalts, 248, 253 bathyalflysch, 91 I AlpineOrogeny, 239 belts of mineralization, 33~ IAlpino-type folds, II bimodal basalt, l8~ IAltay-Hingganling Biogeographical Province, 151 bimodalcharacter, 22~ f'\ltay-Junggar-Ergun Belt, 132 bimodalpattern, 193 IAltay-Junggar-Ergun Early PaleozoicCollisionBelt, 2 bimodalvolcanicrock, 205, 23j f'\ltun ColliSIOn Belt, 105 biogeography, 15q f'\lxa Block, 135 block, 2921 f'\lxa-DunhuangBlock, 105 blocks in the Peri-Gondwanan tectonicdomain, 21 rmalgarnatlOn, 52, 140,367 blocks migration,87 f'\rnount of extension, 251 blocks of the Xiyu tectonicdomain, 21 f'\rnount of shortenmg,251 blocks of the Yangtze tectonicdomain, ~ ~mphlbolite, 213, 240 bottomof lithosphere, 225, 251, 25~ ancient Chinaplatform,66 Bouguergravityanomaly, 315 !indeslte, 193,230 branch fault,225 ~ngular unconformIty, 100, 149 breakupof Rodinia,79 ~ntlclinal folds, 218 broadopen fold, 23~ anticlines, 106 broke up, 71 aqueo-glacialconglomerates, 71 IArchean, 27 CI IArchean continentalnuclei, 31 calc-alkalineseries, 186,205 IArchean oceaniccrust, 37 CaledonianCollisionBelt, 141 rsthenosphere, 318 CaledonianOrogenicPeriod,87 aulacogen.91, 349 catastrophicepisode,367 f'\ustralianPlate, 129, 165 catastrophicfaunaland floralextinctionevent, 149 ~verage rate of E-W extension,250 CathaysianPlate, 2, 59, 60, 63, 87, 92, 1411 ~verage rate of mtraplatedeformatIOn, 163 Central Asian monsoon,2571 ~verage thIcknessof sedImentary systems,51 CentralChma BIOgeographIc Piovmce, 122 fl-94 Index!

~ha' ertai-Langshanzone,56 depthsof magmatism, 2541 Fhalcophile element,350 desert,25] K:hangcheng Tectomc Penod, 51 detachment, 173,177, 191,224, 225,240, 254, 3691 changein the angleof subduction, 193 detachment fault, 20~ changeof coast, 280 detachment sheet, 185 Chinesecontinental lithosphere, II deterioration, 257 klasslficatlOn contmentalcrust, 307 dextral,225, 2321 clockwise rotationof the axes of principal stress,206 dextralstrike-slip, 222 clouds of dust, 376 dextralstrike-slipdisplacement, 25~ Foastlme, 281 dextralstnke-slIpmovement, 232 ~old-water fauna, 127 d[tterenllalstress, 19,210,249, 368 collision, 12, 140,247,291,328 dike swarm,20(j collisionzone, 149,153,349,353 dilation(changes in volume), 121 Follission zoneof Altay-Ergun, 87 disconformity, 103,15! K:olumbla and Rod[masupercontments, 75 discovery of endogemc ore deposits, 35~ Fomposlllon of the mantle,320 d[sperslOn, 247, 367 ~ompresslOn, 221, 232,294 d[splacement, I, 12,240 Fompression axis, 268 displacements of the continental lithospheric plates,291 Fonformable, 239 d[stortlOn (changes m shape), 12 Fonformably, 205 d[stnbutlOn of Aicheancontmental nuclei, 351 ~onJugate shearfracture, 279 d[stnbutlOn of magmatic sourceareas, 187 Fontment-contment collISIOn, 231 dramagebasms,217, 2281 ~ontment-contment collISIOn belt,300 Fontmental crust, 326 Fontmental lIthosphere, 192 dynamiC mechamsm, 259,283, 291, 36~ ontmenta rt os enc mante, ontinentalmar inal extensional basin,259 Fontmental nuclei,34 earliestsedimentary cover,52 conunenral plate,300 Early Cambrian, 51 Fontmental nit zone, 12 Early Ordovician, 90 Fontmental-type crust, 316 Early Paleozoic tectonicperiod, 8~ Fontmental-type IIthosphenc mantle,192 Early Yanshanian, 173 contraction tectonicperiod,374 EarthSciencessystem, ~ FonvectlOn system,369 Earth's rotation,3641 K:ool temperatePen-Slbenan BIOgeographiC Provmce, 126 earthquakes, 267, 27~ rool temperateYunnan-Tibet BIOgeographIC Provmce, East Gondwanacollision,74

1126 EasternTethysPaleo-Ocean, 1421 core, 1 eclogite,65, 18~ Fore-mantle boundary, 372 eclogitebelt, 139 Fosm[c year,8I ecologicalenvironment, 229,257 Founterclockwlse rotation, 173,176, 177, 191,326, 328 ejectivefold systems,221 Cretaceous, 197 elasticdeformation, 296 crocodiletectonics, 301 elasticrebound,202 Frust,28 Emeishanflood-basalt province, 3721 crustal density, 228 Emeishanmantleplume, 121 crustalfault, 350 endogenicore deposits, 339 crustal melting, 193 enrichedmantle,31~ ~rustal shortenmg, 247 environment, 278, 2911 Frustal thickening, 325 Eoarchean, 2] crustal thickness, 192,315,319 Eurasia,231 IEurasIan Plate,2II, 213,231, 232 EuropeanAvalonian, 141 §eep detachment, 22I exogemc, 33~ ~eep lIthosphere fault, 186 ~eformatlOn, I, 12, 179, f99, 219, 351 ~eformatlOn time, 251 extensionfault, 2251 dense fissure belt,227 extensionrate, f63 flensity method,249 extensionvelocities, 381 §epleted mantle,318 extensionzone, 2971 §epresslOn, 227,228, 279 extensIOnal and detachment faults, 22] §epth of magmallc source, f90 extenslOnaf basm,297 IIndex 495 extensionalfault,277 geophysical, 315 ~xtenslOnal faultzone, 227 geophysIcs, ~ ~xtenslOnal jomt system,248 geothermal anomaly, 274 extensional marginal sea, 257 geothermal gradient,36, 43, 60, 67,139,3251 geothermal water,277 Germano-type fold, II [an fold, 300 giant rift system,3241 [ar-fieldeffect,296 giant step, 2541 far-field model,295 glacialconglomerate, 71 farallon Plate, 177 glaucophane faCIes, 240 ~ault, 10,251 globalgravIty field, 36~ ~ault plane solutIOn, 268 globalplate, 3671 ~ault zones,209,254 globaltectonics, 363 [ault-depressionbasin, 297 gneiss,213 [ault-dcprcssion zone, 274,356 Gondwana, 166,212,239,294,3671 OCelSlc granulIte, 23I Gondwanan glaCIal sedIment, 1271 finite expansion of theEarth, 364 lfissure, 277, 351 fissurezone, 278 graniticrock, 205 lfixism, 367 granitoid,18(j Iflood basalt,372 granulite,183 Iflow of flUIds, 277 granulite-gneiss, 31 IflUld content,319 gravitational collapse,24] IflUld mIgratIOn, 35I gravitational equilibrium, 28, 281 Iflysch,231 gravitational isostaticcompensation, 255, 37(j Iflysch (bathyal)turbidite,9 gravity, 36~ [old, 10, 163,267 greenschist, 24q Ifold deformatIOn ume, 224 greenschistfaciesmetamorphism, 103 ~oIded, 210 greenstonebelt, 3~ OColdmg, 291 GrenvilleCollisionZone, 751 ~oldmg deformatIOn trme,198 growthfault,22] Ifolds and thrust, 163 growthtectonicperiod,374 ~olds and thrusts, 163 gypsum, 19] ~ohar structure,291 [oliation, 10 HJ ~oreland basm,239,245, 299 half graben,204 [ormationof coal deposit,230 halite, 19] ~ormatlOn of largefault-depreSSIOn, 204 HarbinPaleoplate, 6] Ifracture, 277 HarbinProtoplate, 58 ~racture reservoir, 278 hardcollision,2311 fupmg Penod, 30 Hercynian(Variscan) CollisionBelt, 141 hi h alkalicontent,20 hi h an Ie reversefault,272 galacticdisc, 81 hIghgravitygradIent, 19~ galacticdisk, 377,379 high mountain, 20~ galacticyear,377, 379 high permeability, 3511 pangdise, 211 fiigf potassium granitemtrusron, 2321 pangdise Block, 104 hIghSIOzcontent,205 pangdise Zone,224 HImalaya, 2171 pangdlSe-Nyamqentanglha Zone,232 HImalayan, 7 panglse Block, 165 HImalayan Block,165 geochemIcal, 3I5 HImalayan Mountams, 2391 geochemIstry, 2 HImalayan movements, 239 geodynamIc environment, 298 HImalayan Plate,73 geologIcal dIsaster, 278 HImalayan tectonicmovement, 2I71 geologIcal hazard,278 HImalayan IectomcPenod, 239, 2941 geologIcal survey, 10 HImalayan Tectonic Zone, 23~ geology,2 Himalayan ThrustZone, 2351 [geomagnetIc pole, 15 Hmgganlmg MongolIa Itanshan CollISIOn Zone, I 6~ geomorphlcal framework, 278 homogeneous, 3701 geomorphology, 254 honzontalcrustalshortenmg, 121 Indexl lJorizontal displacement, 278 Juvenilezone, 7{j lionzontalextension, 12 horizontalmovement, 12 KJ horizontalshearing, 12 K60method,441 Ihot contlllental and and environment, 197 Kazakhstan Plate, 165 liot mantlematenal, 324 liot spot,365 hot spring,277 KunlunBlock, 16~ hotspot,368,369 Kurosegawa Tectonic Zone, 2131 b~draulic fractunng,270 drothermal, 339 LI !iypabyssal porphynes,206 LiHiang Period,38 hypothesisof uniformitarianism, 294 Lancangjiang CollisionZone, 152 landscape, 254 I ~ Lanping-SimaoPalaeogene CollisionBelt, ~ igneousintrusion,232 Lanping-Simao-Indochina Plate, 21 indentation,232 largeigneousprovince, 225 indentatIOn model, 149 largescale baSIC volcamsm, 138 indentationtectonics, 162,301 large-scale expansion of the Earth, 3641 [ndIanOceanPlate,212 Late Cambnan sediment, 90 IIndlan Plate,2, 129,165,211,231, 240 Late Permian-Triassic, 14~ Ilndochllla Plate,232 Late Yanshalllan, 173 [ndosllllan, 7, 294 Late Yanshalllan Penod, 205 [ndOSIllIan IectolllcPenod, 149 latIludmal tectomczone,228 inhomogeneous accretion, 28 Laurasian Super-continental Plate, 141 inner core, 370 Laurentia, 431 lintermediate and lowanglethrusts, 12 leadisotope,66 intermediatepnnclpal stressaxis, 105 IllltersectlOns, 226 intra-contmental extension, 368 linearpatterns,205 [ntra-contincntal orogeniczone,291 linearstrainrate, 198,224, 251 intra-continental platedeformation, 367 lineation, 10 intra-contmental subductIOn, 299 hqUld outercore, 370 intra-continental tectonics, 307 listric, 12 Imtraplate deformatIOn, 87, 149, 158,180,218, 227, 247, listricfault system,2721 291,294 lithophIle element,3501 intraplateextensionmineralization, 352 lithosphere, 1, 186, 31~ Imtraplate extensiontectonics, 339 lithosphere delammatlOn and de-rootmg hypotheSIS, 324 [ntraplatcmagmatism, 232 lithospheric, 32~ intraplateshortening, 193 lithospheric fault,254, 35(J intraplatetype, 225 lithospheric plate, 12,367, 378,379 Ilsostasy, 247 lithosphencthickness, 319 isostatIcanomaly, 281 Indosmmn Tectomc System,149 !sostatlcgravitatIonal compensatIon, 284 localtectomcdetachment, 190 isostaticgravityanomalymap, 282 LoessPlateau,257 lisostatic inequilibrium, 365 low angledetachment, 12 isotope geochemistry, 2 lowangledetachment fault, 1851 !SOtOpIC chronology, 240 lowanglenormalfault,240 IIzanagl Plate, 165,177,294 lowanglethrust, 272 II ow seismicvelocity/ highelectricconductivity layer,369 lowvelocityand highconductivity layer,272, 323 lowercrustalmc1uslOn, 193 lowermantle, II ~~======~==~=~~ I_ower Yangtze region, 9~ M melange, 231, 3001 magmaticintrusion, 1851 magmatIc source, 190,2261 magmatIc sourcearea,207 magmatIsm, 3, 87, 136, 163,218,291 Index 4971

magnetic anomaly, 5 mylonite, 210 !iiagnettc anomaly map, 367 mylomttzed, 185 magnetic lineation, 231 magnitude of differential stress, 163, 221 N r'agmtude of tectomc stress, 181,200 Nadanhada Collision Zone 185 Main Himalayan Thrust Zone, 240 Nanhua Period 67 mantle convecnon, 363, 365 Nanhua Tecton] Period, 511 mantle diapir, 369, 371, 375 nappes, II .. 101 rveo- ~"'y., LL7 ",antle plume, 78, 333, 363, 369, 371, 380 Neoarchean, 27 mantle plume model, 295 Neocathaysian Tectonic System, 173, 180, 21 ",antle plume tectonic period, 374 Neoproterozoic, 51 mantle uplift hypothesis, 299 Neotectonic, 7, 265 ?J.~ ' J' margin of the Sino-Korean Paleoplate, 56 normal fault, 247 marine transgression, 92, 122 normal movement, 225 mathematical model, 355 North American, 141 maximum principal stress axis, 105 North American Continents, 175 mean naleolatitude 17 ,. , 'UJ mean paleomagnetic declination, 17, 175 North American, Baltic and African plates, 141 mechanisms of rock deformation, 291 North China Subtropical-Tropical Biogeographic MedianTectonic Line, 213 Province, 124 ~egascopic, 10 North Sinian, 7 melting noint of rock 190 ",eso-scale fault zone, 352 North Sinian Tectonic System, 217 Mesoproterozoic, 51 North YangtzePlate, 2 metal ore deposit, 206 Northern and Northwest China Biogeographical Province ",etallic mineral deposit, 340 151 metalloaenic belt, 342 etallogemc evolution, 339 metallogenic period, 342 o metallogenic province, 351 obliquity of the ecliptic, 36' etallogenic system, 339 ocean drilling, 231 etallogenic zone, 346 ocean floor, 1 etamorphism, 3, 87, 230, 291 ocean-floor basalt, 227 eteorite crater, 355 oceanic anoxic event, 378 mereorite impact, 363, 379, 380 oceaniccrust, 00, L IU, L)~ ! oceanic lithosphere, 231,319 mereorite impact crater, 375 miarolitic structure 206 oceanic lithosphere mantle, 225, 328 microscopic, 10 oceanic mantle, 3711 ~icrotektite, 377 oceamc mantle material, 2271 Middle and Upper Cambnan depoSit,90 oceamc type, 316 Middle Cambrian-Early Devonian, 87 oceanic-type hthosphenc mantle, 1921 Middle Carboniferous, 90 Ochotsk, 9~ middle crust, 178, 192, 209, 350 Ogcheon, 91 !nigmatites,213 oil and gas field, 271 Imigration of the Earth's poles, 364 oil and gas reservoir, 277 mineral resources, 339 Oiland gas trap, 218 mineralization, 339 Okhotsk Block, 185 ",inimum principal stress axis, 105 mixed crustal and mantle sources, 350 mobilism, 5, 367 Mohorovicic discontinuity, 186, 192,205,209,224,240, ophlOhtemelange, 109 272,323 ophIOlite SUIte, 210, 231 Imoist air masses, 257 OphlOhtlc rock, 185, 1931 !iioist monsoon, 229 ore depOSit, 339 molasse, 9 ore deposits of the iron and platinum groups, 35q Imountain ranges, 228 orogenic period, 2391 ",ultl-penod colhslOn,293 orogenic phase, 4 ~ulti-period of accumulation, 28 overthrust, 12,210 mushroom cloud, 324 overturned, 2221 fl-98 Index!

petrology, 21 faCific Plate, 177, 213,224,294 phases of earthquiike actlVlty,275 Pacific plates and Philippine Sea, 29f1­ Phoenix Plate, 177 palaeogeography, 87 piggyback thrust, 191 palaeomagnetism, 87 planation surface, 2211 faleo-Atlanlic Ocean, 166 plastic deformation, 202, 29~ palco-collision belt, 292 plate collision, 300 paleo-collision zone, 353 plate extension, M, 368 paleo-contmental reconstrucuon, 87 plate movement, 29~ Paleo-Mediterranean Sea, 229 plate tectonic period, 3741 Ipaleo-oceanic crust, 193 plate tectonic theory, 363 raleo-plate, 292 plate tectonics, 36~ faleo-tectonogeographlc reconstruction, 211,233,255 plate-subduction with mantle-delamination hypothesis, Paleo- Tethys Ocean, 132 29<;! Ipaleo-weakness, 183 plates interaction, 284 Palcoarchcan, 30 platform margin, 291 paleobIOlogical dlstnbutlOn, 87 platformal fold belt, 291 Paleocene,197 plume head, 371 raleoclimatology, 2 plume tail, 371 paleoecology, 2 polycyclic, 29j paleogeographic, t4U porphyrite, 20~ paleogeographic reconstruction, 233 porphyry copper deposit, 206 paleogeographic sketch map, 122, 151 post-collision period, 356 paleogeography, 2, 150 post-orogenic extensional collapse hypothesis, 29 paleolatitude, 15 preservation of ore deposit, 352 paleomagnetic, 140,233 principal stress axes, 18 paleomagnetic data, 231,240 principal stress orientation, 197 paleomagnetic declination, 15,209, 233 process of movement, 140 aleomaznetic result 16 000 paleomagnetism, 15,210 Proto-Sino-Korean Plate Tectonic Domain, 54 Paleoproterozoic, 27 proto-wntinental blocks and continental cratonization, 3C Paleoproterozoic period, 38 pull-apart basin, 213, 246 paleotectonic reconstruction, 15, 127, 128,130 pulsating expansion and contraction, 365 paleotectonic sketch, 54, 69, 72 Paleozoic, 1fl-O Pan-African collision 74 Q Pan-African tectonic events, 73,141 Qaiuam Basm, Jjj Pangea, 142,367,379 Qaidam Plate, 165 PangeanSuper Continent, 166,175 Qiangtang Block, 165 para-olatforms, 291 Qiangtang-Gangdise-Himalayan Block, 135 partial decrease oressure, 226 Qianxi Penod, 3U partial fracture, 209 Qilian Aulacogen, 71 partial melting, 247 \,llllan COlliSIOn tselt, [ml Ipartially decreasing, 191 \,llllan Event, lU4 Qnian Tectomc Period, ~71 partially melted and differentiated, 28 .. .. passive contmental margm, 175 Qilian-Altun Collision Zone, 1001 Ipathways, 351 QilIan-Altun Early PaleozOiC colliSIOnbelts, 2 Ipelagicchert, 231 Qilianian, l [Jeri-Gondwanan (Yunnan-Tibet) Biogeographic Province, Qllianshan and Altunshan nit basms, 621 1122 Qmgbmkou Penod, 61 Peri-Gondwanan Tectonic Domain, 54, 61, 63, 69, 72,114, Qingbaikou Tectonic Period, 51 1141 Qmlmg-Dable Belt, 141 Peri-Siberian Biogeographic Province, 122 Qinling-Dabie Block, 65 [Jeri-Siberian Subtemperate Biogeographic Province, 124 Qmlmg-Dable ColliSIOnZone, 1531 !.Jeri-Siberian Tectonic Domain, 2, 54, 61, 63, 69, 72, 112 Qmlmg Dable high pressure metamorphiC belt, 6~ l.Jeri-Yangtze Plate Tectonic Domain, 54, 63, 69 Qmzhou Fangcheng margmal nit areas, 104 period of major collision, 294 quantitative relationship, 275 periodicity, 275 quasI-balance, 294 pen ods ot stability, 367 quasi-contemporaneous penod, 367 petroleum migration, 227 quasi-continental type, 316 petroleum migratIOn and accumulatIOn, 227 quasI-oceanIc type, 31G Index 49'1

IR sedimentary depression, 18~ ~adial crack,371 sedImentary formatIOn, 88 radial displacement, 373 sedimentary thickness, 177,217 radial migration, 379 sedimentation, 87, 121 radial movement of the plate, 327 seismicepicenter, 274 ~adiative platedisplacement, 212 seismicfOCI, 27~ ~adlOlana, 231 seisnucfocusmechamsm solutIOn, 26!l ramp-thrustsystem,300 seismicreflection profile,315 Wate of deposItIOn, 177 seismicsoundmgprofile, 31~ Wate of disperSIOn, 138 seismictomographiC study,240 [ate of extension, 209, 210,251 seisrmcwave,29(J Wate of mtraplatedeformatIOn, 249 shallowmanne sedIment, 1741 rate of intraplateshortening, 209,232 Shangdan-Shangnan-Xinyang-Shucheng CollisionZone] Wate of platedeformatIOn, 209 65 ~ate of platemovement, 87 Shaoxmg ltangshan Zone,641 ~ate of plate shortenmg, 58, 198 Shaoxmg Sh.wandashan ColliSiOn Zone,64, 77, 15~ rate of shortening, 224,273 Shaoxing-Shiwandashan TriassicCollisionBelt, 21 rates of plateextension, 110 shapeof the ore bodies,351 [ates of sea levelnse, 280 sheet-like, 18(J [ates of sedImentatiOn, 57, 88, 217 ShimantoBelt,23!l Wates of shortenmg, 163 shortening, 180,204,225, 230, 2941 ratio betweenhorizontal and verticaldisplacement, 280 shortening magnitude, 198 ratio of extension, 251 shortening rate, 224 ratio of shortening, 251 shortening ratio, 198, 22~ ~e-melted, 186 shoshonite, 247 Weactivated earlierfracture, 305 SHRIMPUlPb analyses,231 recent tectonicstressfield,265,276 reconstruction, 76 [ed clastic sedIment, 197 ~ed Rlver-Jmshajmg stnke-slipfault zone, 232 SibaoTectonic Event,52 regionalangularunconformity, 3 Siberianmonsoon, 257 ~eglOnal petroleum geology, 10 Slbenan Plate, 129, 1651 WegiOnal tectomclineament, 281 Sichuaman, 7, 294 WegresslOn, 92 Sichuanian movement, 197 Welict sea, 229 Sichuanian Tectonic Period, 1971 remote sensing,355 Weverse component, 232 Weverse fault,202, 221, 222 Silurian,91 Weverse movement, 225 Simao-IndochinaPlate, 1651 Weversed fault,267 Sinian,7, 701 ~eologic, 225 SinianTectonic Period,511 Whyolite-trachyte composrtion, 186 sinistralstrike-slip, 210, 218,232, 27~ rIft basm,5.1 sinistralstrike-slip displacement, 242, 2481 rift development, 204 sinistralstrike-slip fault zone, 2131 w.ftmg, 67 Sino-Korean continental protoplate, 381 ring structure,347 Sino-Korean Plate,2,129,135,165 Wock deformatIOn, 3, 10,87, 243 Sino-Korean PlateTectonic Domain,63 ~odmta, 367, 379 Sino-Korean Protoplate,40, 53 Rodiniasupercontinent, 75 Sino-Korean Tectonic Domain,61, 69, 72, 1121 rotationof the Earth, 363 smallintrusion,22:1 IrotatlOn of the stressaxes,209 smalllavasheetsand flows, 2251 Russian-Baltic, 175 smallreversedraganticline,2271 ISmail-scale faultzone, .152 Snow Ball Earth,711 IS solarsystem,81 IS-type, 186,205 solidEarth, II Iscattered mtrusion, 205 Songpan-Garze, 21 Isea floormagneticanomalies, 273 Songshugou OphiOlite SUIte, 65 Isea floormagnetiC anomaly, 259 SouthChmaPlate, 165 Isea-floor spreadmg, 5 South Chma Subtroplcal- lroplcal BiOgeographiC Isedlmentary cover,52, 315 Provmce, 1241 1500 Indexl

South China-TethyanBiogeographical Province, lSI tectonicstress, 178,319 ISouth Yangtze Plate, 2, 60, 87 tectonicstress field,87, 200, 221,249, 254, 291,294 sphere interaction,190 tectonicstress orientation, II spherical structure,28 tectonicsystem,3, 10 spherule, 379 tectonic thrust sheet, 30q Istable (or "umform'J penod, 3, 87 tectomc unit, 342 Istram field, 13 tectomc weakness,3521 stratigraphypaleontology, 2 tectonics, I, 315, 339 strength of lowerlithosphere,319 tectono-magmatism, 173,185,205,230,328 Istrength of the stress, 19 tectono-paleogeographIc reconstruction, 1641 Istress field,218 tectono-stratIgraphIc umt, 3 Istnke-slIp, 210, 225 TemperateNorth Chma BIogeographIC Province, 12~ strike-slipfault, 229, 274 terminaltectonic period, 3741 Istnke-slIp or normalfault,202 terrestnal clastIC rock, 174 Istnke-slIp tectonics,304 terrestnal thermalreglme, 36 Istrong folIatIon, 191 TethysOcean, 175, 193,2111 Istructure, I TethysOceanicPlate, 165 ISturtIan glaCIal penod, 67 that macro-meteorites impact, 3751 IsubductlOn, 12,210, 224, 247 the sourceof metallogemcmatenals, 34~ IsubductIon and compressIOn of Okhotskand Izanagi plate, the theoryof continentaldnft, 12

1173 the Theory of PlateTectonics, I IsubductlOn model,295 the upperand middlecrust, 32~ subducrionof PacificPlate, 225 thermalboundarylayer,31~ IsubductlOn of the lzanagl Plate, 177 thermalregnne, 32~ IsubductIon process, 368 thermodynamics, 3631 IsubductlOn zone, 66 thickeningof the crust and lithosphere,247 Subtropical-tropical South China Biogeographic Province, thicknessof continentalcrust, 44 1126 thicknessof the crust, 315 ISuper CathaysianContinentalGroup,66 thicknessof the lithosphere,192, 25~ Isuper-mantle plume, 177 thin-skinnedtectonicarea, 2721 Isuperplume, 371, 372 thin-skinnedtectonicsystem, 23~ surge tectonics,365 tholeiites,224, 253 Isyn-collision, 356 tholeiiticbasalt, 227 Isyn-sedlmentary fault, 12 Three-dimensional WedgeTectonics, 30I ISyn-sedlmentary or growthfault, 298 thrust, 239 Isyn-tectonic sedimentation, 9 thrust ramp, 2101 Isyncline, 106 thrusting,291 Isyntactlc crust and mantle, 186 TianshanMovement,121 ITianshan Period, 121 ians an- out 10 an 10 e r, Tianshan-South Hin anlin Late Paleozoic Collisio [ailuge Granite,42 Belt, 21 [Iailugetectonic zone,213 Tianshan-South HingganlingTectonicBelt, 100 [IanakuraTectonicLine, 175, 177 Tianshan-South HingganlingTectonicPeriod, 12~ ITancheng Lujiang FaultZone, 162 TIanshan-South HmgganlIng CollISIOn Belt, 121 rrarimBlock, 104, 129, 135 Tianshanian, 7 rrarimPlate, 62, 165 tillite, 671 [lanm, QaIdamand Dunhuang Alxa blocks, 100 tm-nch plate, 601 !ectomc, 140 tomography, 319 !ectonic domain,63, 69, 72 topography, 2541 lectonic event,3 transformation of lithosphere,325 !ectomc evolutIon, 140 tranSItIonal lIthosphere, 192 !ectomc evolutIOn of continents, 12 translatIOn (movements of the rock bodyas a whole), 12 !ectonic framework, 31, 39 transrmssron belt, 36~ lectonic lineament,281 transpressional fault, 186 [Iectomcmap, 154 transtensIOnal fault belt,205 !ectomc penod, 3 trench-arcsystem,231 tectonic reconstruction, 210 trend of fold axes, 198 tectonic sketch, 181,220,244,271 tsunami, 37(1 !ectomc sketchmap, 134 tungsten-nch plate,60 !ectonIcstabIlIty, 205 turbulence,3701 IIndex 501

wedge-shaped oceaniccrust, 259 WestKunlun-Altun-Beishan, 1331 WestPacIfic Palaeogene subductIOn zone,2 Western PacIfic subductIOn zone, 230 westernPacIfic trench arc basmsystem,2571 WilsonCycle, 37~ wrench(strike-slip) fault, 121 Wuchuan-Sihui FaultBelt, 103 WutaiPeriod, 301

xenolith,225 Xlyu Plate, 87, 1411 Xlyu IectonIcDomam, 114 IV YI Ivalue of tectonic stress,270 Yangtze dramagesystem,256 [Varangian glacialperiod,71 Yangtze Plate,63, 92, 135, 141 [variscian or Hercynian Period, 121 Yangtze protoplate, 40 Ivein, 355 Yangtze Tectonic Domain, 112 Ivem systems,355 Yanshan Western LIaonIng RIftBasm,54 IvelocltIes of plate movement, 13 Yanshaman, ] Iveloclty of the Earth's rotation, 364 YanshanIan mtraplatetectono-thermal events, 1781 Ivertical movement, 12 Yanshanian Tectonic Period, 1731 Ivertical uplift,279 Yarlung ZangboCollisionZone,217, 239 Iviscosity, 319 Yarlung ZangboFaultZone,2401 Ivolcanic rock, 186,273 Yarlung ZangboRiverCollisionBelt, 2321 IvolcanIsm, 186 Yarlung ZangboRIver IndusRIverColhslOn Belt, 2311 e ow rver amage, w Yu'nanTectonic Event 10 IW-Sn deposIt, 206 Yuh ShoufengSubductIOn Zone, 2301 ~andashan CollisionZone, 173,177, 185 Yulong Zone,224 ~andashan-West Sikhote-AlinBlock, 185 Yunnan-Tibet ColdBiogeographic Province, 124 Iwarm and moistchmate, 229 Iwarm, humidclimaticcondition,197 ZI Iwater mjectlOn well,278 ZIrcon crystals,23II Iwater-bearing fracturebelt, 277 zonesof tectonicweakness, 2811