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Index to Volume 122 INDEX TO VOLUME 122 This index provides coverage for both the Initial Reports and Scientific Results portions of Volume 122 of the Proceedings of the Ocean Drilling Program. Refer- ences to page numbers in the Initial Reports are preceded by “A” with a colon (A:), and those in the Scientific Results (this book), by “B” with a colon (B:). The index was prepared by Wm. J. Richardson Associates, Inc., under subcontract to the Ocean Drilling Program. The index contains two hierarchies of entries: (1) a main entry, defined as a key word or concept followed by a reference to the page on which that word or concept appears, and (2) a subentry, defined as a further elaboration on the main entry followed by a page reference. The index is presented in two parts: (1) a Subject Index and (2) a Taxonomic Index. Both parts cover text figures and tables but not core-description forms (“barrel sheets”) or core photographs. Also excluded are bibliographic references, names of individuals, and routine front and back matter. The Subject Index follows a standard format. Geographic, geologic, and other terms are referenced only if they are subjects of discussion. This index also includes taxonomic entries above the generic level, as well as broad fossil groups such as foraminifers and radiolarians. The notation “ff” following a page listing indicates that reference to a topic continues beyond the last page given but is not sequential. This would be the case where one or more figures or tables follow a principal topic of discussion that makes up a major section. A site chapter in the Initial Reports is considered the principal reference for that site and is indicated on the first line of the site’s listing in the index. Such a reference to Site 762, for example, is given as “Site 762, A:213-288.” The Taxonomic Index is an index relating to significant findings and/or substantive discussions, not of species names per se. This index covers three varieties of informa- tion: (1) individual genera and species that have been erected or emended formally, (2) biostratigraphic zones, and (3) fossils depicted in illustrations. A taxonomic entry consisting of both genus and species is listed alphabetically by genus and also by species. Biostratigraphic zones are listed alphabetically by genus; zones with letter prefixes are listed under “zones.” For further information, including available electronic formats, contact the Chief Production Editor, Ocean Drilling Program, 1000 Discovery Drive, College Station, Texas 77845-9547, U.S.A. 912 Index to Volume 122 SUBJECT INDEX acoustic basement, Exmouth Plateau, B:75–76. Atlantic Ocean South, A:240; B:659, 661 terrigenous origin, A:261 See also basement Australia thermal maturity, A:248; B:312 Adenet limestone, Northern Calcareous Alps, Barrow Island, A:236 truncation, B:77 B:782 Carnarvon Basin, B:221, 233-237, 803 volcanic detritus, B:252 Africa N, tectonic map, B:84 Cretaceous–Cenozoic hiatuses, B:289 Barrow Island, A:236 Alabama, Cretaceous marl-limestone sequence, plate tectonics, B:272 basalts, Wallaby Plateau, B:225–226 B:259 rifting, B:11 basement Albian/Cenomanian boundary, calcareous nanno- separation from Greater India, B:224 Argo Abyssal Plain, B:787 fossils, A:240 Australian margin Exmouth Plateau, B:75–76 algae, Rhaetian, B:166 Aptian-Albian sedimentation, B:101 basement, volcanic, B:70-71, 73-74, 77, 79 algal mats, A:206; B:114, 200. See also sedimen- breakup history, B:83, 85 belemnites tary structures Cenozoic-Cretaceous sediments, B:766 age, B:220, 789 alkalinity, A:106, 150, 194, 261, 333 collision, Indonesian crustal collage, B:57 origin, B:576-577 calcite dissolution and, B:306-307 depositional environment, B:92 paleoecological implications, B:573, 575 Exmouth Plateau, B:297 fluviodeltaic sediments, B:225 Site 761, A:179; B:584-585 organic carbon content and, B:303 Jurassic marine sediments, B:96 Site 763, A:304, 306 alkanes paleogeography, B:215, 788-789, 791 stable isotopes, B:572–576 Cenomanian/Turonian boundary, B:323, 332 rifting, B:56-57, 101–102 Benguela Upwelling System, salinity, B:662 Exmouth Plateau, B: 322, 331 seafloor spreading, B:768 Bentong-Raub suture, age, B:86 marine-dominated vs. land-derived, Tethyan evolution, B:766-768 bentonite B:856-857, 859 Triassic sedimentation, B:93, 96 Barrow Group, B: 225, 242 Site 759, B:327 Australian Northwest Shelf biostratigraphic age, B:220 Site 765, B:333 carbonate dissolution, B:51 with calcispheres, B:232 Wombat Plateau, B:319, 327 carbonate reefal platforms, B:35 definition, B:213 Alpine Orogeny, B:86 heat flow, B:363 deposition as ash turbidites, B:226 Alps, Northern Calcareous, B:782 mudstones, B:6 distance from source area, B:227 Alps, Western, paleostress reorientation, B:209 regression, B:253 Exmouth Plateau, B:13 alteration, diagenetic. See also diagenesis sandstones, B:6 genetic origin, B:222, 224 Cretaceous cyclic sediments, B:262-263, 268 Triassic sedimentation, B:10 geochemistry, B:218-219, 222, 224 oxygen isotopes, B:576, 658 authigenesis, noncalcareous, B:146. See also dia- horizons B1–B6, B:216, 220-221,789 post-depositional uplift, B:150 genesis horizons B2–B6, B:229-230 syn-Rhaetian cyclic emersion, B:149–150 mineralogy, B:222 Althgarh basin, Aptian–Albian sedimentation, bafflestone, B:156, 186 pure vs. impure, B:221 B:98 Banggong Co–Nu Jiang ocean, B:88 sedimentary and tectonic settings, B:224-225 alumina, B:866-867, 873–875, 878-879 Banggong Co–Nu Jiang suture, B:96 sedimentary fabric, B:221 aluminum barium in silty claystone, B:220 in ferromanganese deposits, B:339-341 anoxic reducing condition, B:305 Site 761, A:167, 179, 208; B:229 geophysical well logging, A:202-203, in ferromanganese deposits, B:339-341 Site 763, A:306, 349 284-285; B:384 in Leg 122 sediments, B:302 smectite, B:222, 231–232, 789 aluminum oxide. See alumina Barranco del Gredero (Spain), Cretaceous/Ter- stratigraphic context, B:215–216, 220 Alxa basin, Jurassic sedimentation, B:96 tiary boundary, B:743 volcaniclastic origin, B:224, 225, 789 Alxa block, Triassic fluviolacustrine sediments, Barrow-Dampier basin, Callovian–Tithonian un- benzofluoranthene, Wombat Plateau, B:321 B:93 conformity, B:207 Berriasian/Valanginian boundary, B:807 Alxa–North China block, Permian sedimentation, Barrow delta system, B:77, 79-80 bindstone, B:147, 155 B:88 Barrow Group biocalcarenite, sparry, B:464 ammonite, Site 763, A:303, 305–306 age, A:241, 318; B:40, 539-540 biolithite facies, microfacies types, B:143 anastomosing seams, Site 762, A:233–234, 281 alkalinity, A:261 biostratigraphy. See Taxonomic Index for genera anisotropy, A:107, 371 bentonite, B:225, 242 and species; Subject Index under particu- Annamia block, B:92, 93, 96 coarse fraction components, B:238, 239, 241, lar fossil groups and sites Antarctic Bottom Water (AABW), erosional ef- 244 biotite, Site 761, B:231 fects of, B:792 deposition, B:559, 561, 806 Birdrong Sandstone, B:216, 252-253 apatite, euhedral, B:231 Exmouth Plateau, B:9, 238–239 birdseye structures, in Rhaetian limestones, Argo Abyssal Plain. See also Indian Ocean formation, B:13, 253, 814 B:114, 187 formation, B:3, 6, 13, 803 geologic setting, B:236 bitumens, compounds in extractable, B:329–330 lithostratigraphy, A:376 geophysical well logging, A:286; B:245, 385 bituminite. See torbanite magnetic anomaly, B:784 high-molecular-weight hydrocarbons, A:250 Black Sea, A:240; B:661 north-south cross section, B:767 microfossils, B:559–560 Bonaparte Gulf Basin, B:92 ocean crust, A:9 mudstones, B:255, 257 Bongthol Tangla block, B:96 organic geochemistry, B:324 organic matter, B:312 boundstone seafloor spreading, A:5, 207; B:786-787 petrology, B:242, 244, 246 coral, A:360; B:156, 166, 177, 186 tectonic influences, B:224 progradation, B:805 coralline red algae, B:175 Argo Landmass salinity, B:306 diagenesis, B:149 breakup from Exmouth Plateau, B:805, 814 sedimentation rate, B:815 hematite-stained, B:164, 166 Laurasian accretion, B:787, 789 seismic reflection profiling, B:47, 70 red sponge, B:183–186, 839 ash, Cretaceous post-breakup, B:225 seismic sequence correlation, A:271, 345–346 tabulozoan/bryozoan, B:186 ash layer, B:226-227 shallow-marine to intertidal environment, vermiform texture, B:168 Ashmore platform, B:93 B:825 boundstone, calcisponge-brachiopod, B:202 astrorhizids, B:559 Site 762, A:216-217, 236, 348–349 boundstone, coral, B:202 Ataxophragmiidae, Site 764, B:435 Site 763, A:289-291 boundstone/rudstone, with coral and coralline al- Atlantic Ocean North, A:240 source region, B:40, 244, 251–252, 803 gae, B:178 913 Index to Volume 122 Braarudosphaera SUBJECT INDEX Braarudosphaera. See Taxonomic Index paleoecological implications, B:573, 575 Cenomanian/Turonian boundary, B:312 braided stream deposits, in delta systems, B:775 Site 761, B:581 in glauconitic grains, B:852 Brazos River, Cretaceous/Tertiary boundary, stable isotopes, B:572–574 light vs. dark beds, B:261, 267 B:743 calcisponges, B:140, 142, 190-191 Site 759, A:101 breccia, conglomerate/shell, Carnian/Norian calcite deposits Site 760, A:142 boundary, B:772 clear, isotopic composition, B:846 Site 761, A:190, 193–195 breccia, tectonic, Wombat Plateau, B:133 cloudy, in Megalodon shell, B:848–849 Site 762, A:248, 252-258, 283; B:313 Brianconnais Zone, Wombat and Exmouth Pla- Cretaceous/Tertiary boundary, B:758 Site 763, A:321, 325; B:313 teau compared, B:208 in ferromanganese deposits, B:337 sulfate content and, B:303 Brigadier Formation, B:39, 46, 314 geomorphic, in Megalodon shell, B:849 vs. hydrogen index, B:311-312, 314 Brunhes Chronozone, Site 763, A:318 calcium
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  • Upper Devonian Deposits At. G6rno in the Holy Cross M Ts

    Upper Devonian Deposits At. G6rno in the Holy Cross M Ts

    .: .......; ': aCla' :" geologlca polonica Vot 31. No. 3-4 . :; ... KRlZYBZTOF MALKOWSKJ Upper Devonian deposits at . G6rno In the Holy Cross M ts ..,' '1 · ' . -.. .. '. ; .. ~ ~ : , . .. AlBS'IlRA.OT: The lith010gy af the Upper lDevionian >oarobona'te deposits of the· -e:nvlTons off Gor.no, alo.ni· wiih .thed.r oonc.doni Stratigra,phy ga.ve a ibaSis ror reco­ gniti'On af the Sedimen'ta'i!ion and pa:leogeography ·of the lI'egtcm wJ.1ftun .\the Upper'. Dev.onian ibasiJll of the Holy OrQSS Mts. The tecto.ni<: gaPs reoognized between 1he ' Givetian and FrasnJi.an. as well as !between the Devonian and Cal1borllil£erous depo­ sits, led ,t.o the .corredti,OiIl.s in the r~to.nalJ. tectonics.. Three S'pedi.es .()f oonodoms, viz. Polygnathus ancyrognathotde1LS Zieg1er, Schmidtognatnu.s aff. pietzneri Ziegler and Spath,ognathodu.s sannemanrrr;i treptv.s lZiegler, s·o far unknown Ifrom the De- vQ.IlJian 'Of the lHoIJ.y Oross Mts. halVe 'been described. :.: , " ,., iNrnoDuCTION .' .. ', .. :... ~ , . .;": ' ... ~.: .. .. .'. ~ne!a!l stra!ti.:gxaphicframework, based on the COI1J9Clonts, . was . pr-e- . sent~ Jor the Upper Devonlian d€lposits of the Holy croSs ,Mts by g.Z'Ui~ czewsJ9.:(19711).The sicoipe Olf the pre£'ent 'contrllbu1li.oJ:?. is to, apply .'the ~noqon't straltigraphy to a more detailletd recognition of !the p.rach~n~· , t~~lill.e. ·. of yar.nlo, lhaviingacomplex tectonic sb-uCi1nlre' an ith~ centx-aLpart ~ .t}},~,Holy Gross.iM'ts. I(se~ rr~-1i;g. 1; and IMallkowski 19U); ,Mosl; : ~SO far , avaia.ab)re~ dataon Ithe strat~phy a~fac1;€S deV1el~t , Of ~ Itll:e :P ,~N1OIl4aIl deposiltsin ~ larea .come from~IOOlalIwOTks .oov'~ring -e2d;ep.- .
  • Eastern Anti Atlas Phanerozoic Granular Iron Formations (Ifs): Nomenclature and Classification, Case of Ordovician Basin of Tafilalt

    Eastern Anti Atlas Phanerozoic Granular Iron Formations (Ifs): Nomenclature and Classification, Case of Ordovician Basin of Tafilalt

    Available online www.ejaet.com European Journal of Advances in Engineering and Technology, 2016, 3(12): 30-38 Research Article ISSN: 2394 - 658X Eastern Anti Atlas Phanerozoic Granular Iron Formations (IFs): Nomenclature and Classification, Case of Ordovician Basin of Tafilalt Saoud N1, Charroud M1, Dahire M2, Hinaj S1 and Mounir S1 1Laboratory of Georesources and Environment, Faculty of Sciences and Technologies, Sidi Mohammed Ben Abdellah University, Fez-Morocco 2 Laboratory of Geodynamics and Natural Resources, Faculty of Science Dhar el Mehrez, Sidi Mohammed Ben Abdellah University, Fez-Morocco [email protected] _____________________________________________________________________________________________ ABSTRACT In Morocco, the variety of ferruginous resources (dated Archean, Paleozoic and Mesozoic) shows a specific char- acter illustrating the relationship between the geographic position and the geodynamic setting which allows depo- sition of several iron mineralized structures. The sedimentary iron is well manifested in the Paleozoic terranes, and assigns great relation with the Hercynean geodynamic regime, which marks the Gondwanean environment during this time. The results of these processes manifest as the establishment of exploitable iron Formations depos- it situated in the Tafilalt Ordovician basin of the eastern Anti Atlas of Morocco. Key words: Hercynean, Gondwanean, exploitable iron deposits, Tafilalt Ifs, Ordovician, Anti Atlas, Morocco _____________________________________________________________________________________ INTRODUCTION Iron Formations (IFs) originates from sedimentary deposition processing, and they are characterized by a high grade iron tenor which manifest as tiny or laminated chemical facies and contains more than 15% sedimentary iron. The ore is formed by iron oxides and hydroxides such as hematite (Fe2O3) and magnetite (Fe3O4) both consti- tute the major part of the mineralized rock.