Sheet 3 of 4 U.S

Total Page:16

File Type:pdf, Size:1020Kb

Sheet 3 of 4 U.S ETAL S, M LOG E EN RC E U S O IS S , E T E R C L T A O R N E I C N I S M R S A S G , S M U A J, S, S JU M, G N , KIGA OR IA THEAST AS Prepared in collaboration with Scientific Investigations Map 3022 U.S. Department of the Interior Russian Academy of Sciences, Mongolian Academy of Sciences, Jilin University, Korean Institute of Geoscience and Minerals, Sheet 3 of 4 U.S. Geological Survey Geological Survey of Japan/National Institute of Advanced Industrial Science and Technology Pamphlet accompanies map 75° 75° 82° 144° 82° 144° 84° 82° CAMBRIAN THROUGH SILURIAN (540 to 410 Ma) METALLOGENIC BELTS 84° 82° DEVONIAN THROUGH EARLY CARBONIFEROUS (MISSISSIPPIAN) 96° 132° [Listed north to south, progressing west to east; see table 3 for summary of metallogenic belts; belt label in red] 96° 132° 108° 120° 108° 120° (410 to 320 Ma) METALLOGENIC BELTS [Listed north to south, progressing west to east; see table 3 for summary of metallogenic belts; belt 80° 80° Label Belt Name Country and (or) Region 80° 80° label in red] Tuo Tuora-Sis Russia,Yakutia ea ea BED Bedobinsk Russia, Eastern Siberia (Yenisey Ridge area) Label Belt Name Country and (or) Region vor la vor la TK Taidon-Kondomsk Russia, Southern-Eastern Siberia (Kuznetsk Alatau Mountains) UD Udzha Russia, Northeast Yakutia MT Martaiginsk Russia, Southern-Eastern Siberia (Kuznetsk Alatau, DO Daldyn-Olenyok Russia, Northeast Yakutia sl Gorny Altai Mountains) sl OR Orulgan Russia, Northeast Yakutia 76° 76° 76° 76° ksh la Kiy Kiyalykh-Uzen Russia, Southern-Eastern Siberia (Kuznetsk Alatau Mountains) ksh la Bot Botuobiya -Markha Russia, Central Yakutia KK Kizir-Kazyr Russia, Southern-Eastern Siberia (Eastern Sayan Ridge) ubn CTC sl ubn CTC sl SD Sette-Daban Russia, Southern Yakutia NS North-Sayanian Russia, Southern-Eastern Siberia [West Sayan Mountains] MCh Mamsko-Chuiskiy Russia, Northern Transbaikalia kr KY KhK Khemchik-Kurtushi-binsk Russia, Southern-Eastern Siberia (Tuva area) kr KY KR ut KY pl KR ut KY pl Sn Synnyrskiy Russia, Northern Transbaikalia CTF Ondumsk Russia, Southern-Eastern Siberia (Tuva area) CTF lch kr ON lch kr Bod Bodaibinskiy Russia, Northern Transbaikalia lch NAT UO Ulugoisk Eastern Tuva, West Siberia, Russia lch NAT Muiskiy Russia, Northwestern Transbaikalia CTK sl SH CTK sl SH MS 72° CTM 72° 72° CTM 72° NAT CTC ly Iiskiy Russia, Southern-Eastern Siberia (East Sayan area) NAT CTC Ber Berdsko-Maisk Russia, Southern-Eastern Siberia (Salair Range) B-K Bokson-Kitoiskiy Russia, Southern-Eastern Siberia (East Sayan) SL Salair Russia, Southern-Eastern Siberia (Salair Range) pl OZ Ozerninsky Russia, Western Transbaikalia pl Ksh Kiya-Shaltyr Russia, Southern-Eastern Siberia (Kuznetsk Alatau pl Krh Kruchi-ninskiy Russia, Northeastern Transbaikalia pl Mountains) nw KNG KOV ShG Shimanovsk-Gar Russia, Far East nw KNG KOV SO Sorsk Russia, Southern-Eastern Siberia (Kuznetsk Alatau Uda-Shantar Russia, Far East Mountains) KN pl UdS KN pl tup pp KPD tup pp KPD 68° Tuo 68° UT Uzuurtolgoi Western Mongolia 68° 68° TE Teisk Russia, Southern-Eastern Siberia (Kuznetsk Alatau DL DL UD KH KNG mr HO Hovd Western Mongolia KH KNG mr Mountains) ktk ktk tup zr tup zr Chapsordag Russia, Southern-Eastern Siberia KOV TG Tastyg Russia, Southern-Eastern Siberia (Southern Tuva area) KOV ChD pk pk NAV ad TL Telmen Northern Mongolia NAV ad AG Agulsk Russia, Southern-Eastern Siberia (Eastern Sayan) KPD ZJ Zavhanmandal-Jargalant Central Mongolia KPD KZ Kizhi-Khem Russia, Southern-Eastern Siberia (Northeast Tuva area) OR RA Rudny Altai Russia, Southern-Eastern Siberia MG ktk KPD Kch Khachim- gol Northern Mongolia MG ktk DO KPD 64° KN 64° KN KKh Korgon-Kholzun Russia, Southern-Eastern Siberia (Gorny Altai area) NAC 64° EG Egiingol Central Mongolia NAC 64° Bgl Bayangol Central Mongolia SH Shirgaita Russia, Southern-Eastern Siberia (Gorny Altai area) tk tk Zaa Zaamar-Bugant Central Mongolia DS Deluun-Sagsai Western Mongolia tuv tuv KhZ Khalzan-burged Western Mongolia NAV Chn Chagoyan Russia, Far East NAV oc S-Kh South Khingan Russia, Far East oc BK Bayan-Kol Russia, Southern-Eastern Siberia (Tuva area); Northern tup BH-1 Bayanhon-gor-1 Central Mongolia tup Mongolia OH GAl Govi-Altai Southwestern Mongolia OH BOM Bugseingol-Ovormaraat Northern Mongolia 60° 60° 60° 60° tup nw oc IB Ikh Bogd Central Mongolia tup nw oc TN Tomurtein Nuruu Southwestern Mongolia Bdz Bidzhan Russia, Far East OH TY Tamirgol-Yoroogol Central Mongolia OH ob ob BAN Baruunhuurai Southwestern Mongolia oc XL Xilin Northeastern China oc JX Jixi Northeastern China SD HAN Hangai Central Mongolia nw vch nw vch Bot WAG TD Tadong Northeastern China WAG ED Edrengiin Southwestern Mongolia NAV ud NAV ud NAC Kb Kabarga Russia, Far East NAC BG Bayangovi Southern Mongolia 56° CA NAC 56° CA NAC IS NAC 56° IS NAC 56° BL Bayanleg Southern Mongolia BED os VZ Voznesenka Russia, Far East os ta NAV ta NAV UZ Ulziit Southern Mongolia oc BN Bainaimiao North-Central China oc vch vch EBT dz FN Fangniugou Northeastern China EBT dz Sul Sulinheer Southeastern Mongolia NAC NAC Bod WAG tuv NAP EUC WAG tuv NAP EUC Heg Hegenshan Northeastern China NAE TF WAD oc HT Hunjiang-Taizihe Northeastern China NAE TF WAD oc TT YN ul GL TT YN ul GL nw NR am CAL nw NR am CAL YA Yaroslavka Russia, Far East dz JZ Jinzhong Northern China dz SAL tn KZ sab sab SAL tn KZ sab sab EZ Edren-Zoolon Southern Mongolia 75° kt CH ud EL East Liaoning Northeastern China 75° kt MChCH ud KUV bv BM cuk tr tr st Ksh KUV bv BM cuk tr tr st OD sab Ber OD sab TsS Tsagaan-suvarga Southeastern Mongolia MT bv st kl ko 52° bv st kl ko 52° 52° ak ua st es ns 52° ak ua st es ns kh mn st st to UdS kh mn st st to HQ Hongqiling Northeastern China nw ag CAL GL ZRA nw ag CAL GL ZRA kz bk dz kz SO bk dz AL ma TZ BM TY st vz GL kni AL SL ma TZ BM TY st vz GL kni MR TK ss KK DR CAL UB LN SS MR ss AG DR MS CAL UB LN SS CHR Kiyas KA ss NAC UN la CHR as KA ss NAC UN la ACH UL KK sa BM BRG se TD uo ha TR KKhACH UL KK sa BM SnBRG se TD uo ha TR 78° al mn Iy se TD 78° TEal mn se TD as bv kd kbu as bv kd kbu MT tn NRS se WST es WSA sk tn NRS se WST es WSA sk UK az uo EXPLANATION UK az uo RA trb RA HS trb KBN al HM la OL ShG BD KBN al HM la OL BD KRT as nw OI bv MM ChDKRT as nw OI bv MM bl ba DZEKhK UO NAP hr 48° [Refer to Sheet 1 for list of map units] RA bl ba DZE NAP hr 48° NSWSY tn BI SHA bk bk AR bu WSY tn BI SHA bk AR bu al ss BK OZ AR AR ko ca wsa al KZ ss BK bk AR AR ko ca wsa khs trb ga trb az Chn es SS khs trb ga trb az es SS BR UO B-K bv trb gh tbr sj TERRANES IN LATE PRECAMBRIAN AND PHANEROZOIC OROGENIC BELTS BR UO bv trb gh tbr sj kb tv kb tv TK OM ss hb gh UR TK KKh OM ss hb gh UR ON kbu ha sk Cratonal terrane BOM kbu ha sk 84° al la TU trb trb ha 84° al la TU trb trb ha TG HM tl ND sol ZRA ANV KhZ HM tl ND sol ZRA ANV sal am HU la Kch trb OSKrh trb sal am HU la trb OS trb UzuAT SA te bv trb ub ko SMA WSA AT SA te bv trb ub ko SMA WSA SA lb ji MK os Passive continental margin terrane SA lb ji MK os DZ ji S-Kh DS DZ ji Bdz 48° tl se am AR ags gh ca sj jh 48° tl se am AR ags gh ca sj jh EG tl zhs zg 44° tl zhs zg 44° LK TL kbu es jn Continental margin turbidite terrane LK kbu es jn te BY tl OI ko BK te BY tl OI ko al HO BY hg ca ca jh TN al BY hg ca ca jh TN ZA Bgl se OS gh gh HE NA jn ZA se OS gh gh HE NA jn al gh zhs Continental margin arc terrane al gh zhs zh hg mt trb ji JI Kb zh hg mt trb ji JI QT ZJ hlt yj jn SHM QT HAN hlt yj jn SHM gl tl Zaa AR trb gh XL JX gl tl AR trb gh zh MO kbu vl MO kbu vl HV se gh HL jv Island arc terrane HV se zh gh HL jv OS HD gh MO sol JI OS HD gh MO sol JI WB DN ca ZN la sg es WB DN ca ZN la sg es LK HD mt LK HD mt hg OI mt GA VS jn BAN hg OI mt GA VS YA jn TY trb gh trb ca Oceanic terrane and oceanic crust of oceans trb gh trb ca hg tg trb dxs ZN us 40° hg tg trb dxs ZN us 40° 90° BH-1 am ktb jb 90° ED am ktb jb bw BY trb sm zhs ji ji vl TH bw BY trb sm zhs ji ji vl TH hx am gh ID DN VZ Accretionary wedge terrane, type A- dominantly turbidites with lesser or hx am gh ID DN am ID mt trb trb jn MC am ID mt trb Heg trb jn MC Gal sm jh LG no oceanic rocks BG sm jh LG WB GA trb GA el SL jh SG WB GA UZ trb GA el SL HQ jh SG bw hx trb MO TD bw hx trb MO ED BG GA ca LA jv Accretionary wedge terrane, type B- dominantly oceanic rocks with ED BG GA ca LA jv IB MO GS MO DN LA SK MO GS MO DN LA SK WB MN dxs SKJ WB MN dxs SKJ BA trb GS el FN nm JT lesser turbidites BA trb GS el nm JT trb yl ca db BL trb yl ca db sm trb lg trb el ej jv sm trb lg trb el ej jv ZO sm skc slj os Metamorphic terrane ZO sm skc slj os trb BA HX jl EZ trb BA HX jl HX SL slj yj hi 36° TN HX SL slj yj hi 36° 96° TG SL BN yl skc os jn 96° TG SL yl skc os jn np BA dms nm dxs SKM TERRANES IN EARLY PRECAMBRIAN CRYSTALLINE BASEMENT OF np BA dms nm dxs SKM nm SKR nm SKR trb lg WD HT db jv trb lg WD db jv XC zbl SKL db chs MC CRATONS AND CRATONS WITH MIOGEOCLINAL OVERLAP XC TsS Sul zbl SKL db chs MC trb nm ca slj trb nm ca slj SKE SKL jq SKE SKL jq ed SKE yl jn ed SKE yl jn zbl ay db jn Granite-greenstone terrane zbl ay db jn SKA zbl SKL jn SKA zbl SKL jn 40° yl skc yl MC pb 40° yl skc yl MC pb SKYS skc ldp nr NN SKYS skc ldp nr NN nm skc SKR Tonalite-trondhjemite-gneiss terrane nm skc SKR SKA SKJEL chs jn jq hi SKA SKJ chs jn jq hi sgg MC jv sgg MC jv IM 32° IM 32° 102° snw SKYE Granulite-orthogneiss terrane 102° snw SKYE SKL SCG hi nr SKL SCG hi nr skc ed OG os skc ed OG os ht SKL nc AMAM hi jq hi SHM ht SKL nc AMAM hi jq hi SHM SKJ SCG Granulite-paragneiss terrane SKJ SCG nr os nr os fh skc skc SCJ yc AM fh skc SCJ yc AM os ky SW skc os ky SW JZ ly ib 144° Paragneiss terrane ly ib 144° jn jn 108° 114° 120° MC NN
Recommended publications
  • North and Central Asia FAO-Unesco Soil Tnap of the World 1 : 5 000 000 Volume VIII North and Central Asia FAO - Unesco Soil Map of the World
    FAO-Unesco S oilmap of the 'world 1:5 000 000 Volume VII North and Central Asia FAO-Unesco Soil tnap of the world 1 : 5 000 000 Volume VIII North and Central Asia FAO - Unesco Soil map of the world Volume I Legend Volume II North America Volume III Mexico and Central America Volume IV South America Volume V Europe Volume VI Africa Volume VII South Asia Volume VIIINorth and Central Asia Volume IX Southeast Asia Volume X Australasia FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS UNITED NATIONS EDUCATIONAL, SCIENTIFIC AND CULTURAL ORGANIZATION FAO-Unesco Soilmap of the world 1: 5 000 000 Volume VIII North and Central Asia Prepared by the Food and Agriculture Organization of the United Nations Unesco-Paris 1978 The designations employed and the presentation of material in this publication do not irnply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations or of the United Nations Educa- tional, Scientific and Cultural Organization con- cerning the legal status of any country, territory, city or area or of its authorities, or concerning the delirnitation of its frontiers or boundaries. Printed by Tipolitografia F. Failli, Rome, for the Food and Agriculture Organization of the United Nations and the United Nations Educational, Scientific and Cultural Organization Published in 1978 by the United Nations Educational, Scientific and Cultural Organization Place de Fontenoy, 75700 Paris C) FAO/Unesco 1978 ISBN 92-3-101345-9 Printed in Italy PREFACE The project for a joint FAO/Unesco Soil Map of vested with the responsibility of compiling the techni- the World was undertaken following a recommenda- cal information, correlating the studies and drafting tion of the International Society of Soil Science.
    [Show full text]
  • Siberia, the Wandering Northern Terrane, and Its Changing Geography Through the Palaeozoic ⁎ L
    Earth-Science Reviews 82 (2007) 29–74 www.elsevier.com/locate/earscirev Siberia, the wandering northern terrane, and its changing geography through the Palaeozoic ⁎ L. Robin M. Cocks a, , Trond H. Torsvik b,c,d a Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK b Center for Geodynamics, Geological Survey of Norway, Leiv Eirikssons vei 39, Trondheim, N-7401, Norway c Institute for Petroleum Technology and Applied Geophysics, Norwegian University of Science and Technology, N-7491 NTNU, Norway d School of Geosciences, Private Bag 3, University of the Witwatersrand, WITS, 2050, South Africa Received 27 March 2006; accepted 5 February 2007 Available online 15 February 2007 Abstract The old terrane of Siberia occupied a very substantial area in the centre of today's political Siberia and also adjacent areas of Mongolia, eastern Kazakhstan, and northwestern China. Siberia's location within the Early Neoproterozoic Rodinia Superterrane is contentious (since few if any reliable palaeomagnetic data exist between about 1.0 Ga and 540 Ma), but Siberia probably became independent during the breakup of Rodinia soon after 800 Ma and continued to be so until very near the end of the Palaeozoic, when it became an integral part of the Pangea Supercontinent. The boundaries of the cratonic core of the Siberian Terrane (including the Patom area) are briefly described, together with summaries of some of the geologically complex surrounding areas, and it is concluded that all of the Palaeozoic underlying the West Siberian
    [Show full text]
  • Corel Ventura
    Russian Geology and Geophysics 51 (2010) 322–327 www.elsevier.com/locate/rgg Permo-Triassic plume magmatism of the Kuznetsk Basin, Central Asia: geology, geochronology, geochemistry, and geodynamic consequences M.M. Buslov a,*, I.Yu. Safonova a, G.S. Fedoseev a, M. Reichow b, K. Davies c, G.A. Babin d a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, prosp. Akad. Koptyuga 3, Novosibirsk, 630090, Russia b Leicester University, University Rd., Leicester, LE1 7RH, UK c Woodside Ltd., St. George St. 240, Perth, WA 6000, Australia d FGUP SNIIGGiMS, Krasnyi prosp. 67, Novosibirsk, 630091, Russia Received 14 February 2008; received in revised form l8 December 2009 Available online xx August 2010 Abstract The Kuznetsk Basin is located in the northern part of the Altay–Sayan Folded Area (ASFA), southwestern Siberia. Its Late Permian–Middle Triassic section includes basaltic stratum-like bodies, sills, formed at 250–248 Ma. The basalts are medium-high-Ti tholeiites enriched in La. Compositionally they are close to the Early Triassic basalts of the Syverma Formation in the Siberian Flood basalt large igneous province, basalts of the Urengoi Rift in the West Siberian Basin and to the Triassic basalts of the North-Mongolian rift system. The basalts probably formed in relation to mantle plume activity: they are enriched in light rare-earth elements (LREE; Lan = 90–115, La/Smn = 2.4–2.6) but relatively depleted in Nb (Nb/Labse = 0.34–0.48). Low to medium differentiation of heavy rare-earth elements (HREE; Gd/Ybn = 1.4–1.7) suggests a spinel facies mantle source for basaltic melts.
    [Show full text]
  • Defining Territories and Empires: from Mongol Ulus to Russian Siberia1200-1800 Stephen Kotkin
    Defining Territories and Empires: from Mongol Ulus to Russian Siberia1200-1800 Stephen Kotkin (Princeton University) Copyright (c) 1996 by the Slavic Research Center All rights reserved. The Russian empire's eventual displacement of the thirteenth-century Mongol ulus in Eurasia seems self-evident. The overthrow of the foreign yoke, defeat of various khanates, and conquest of Siberia constitute core aspects of the narratives on the formation of Russia's identity and political institutions. To those who disavow the Mongol influence, the Byzantine tradition serves as a counterweight. But the geopolitical turnabout is not a matter of dispute. Where Chingis Khan and his many descendants once held sway, the Riurikids (succeeded by the Romanovs) moved in. *1 Rather than the shortlived but ramified Mongol hegemony, which was mostly limited to the middle and southern parts of Eurasia, longterm overviews of the lands that became known as Siberia, or of its various subregions, typically begin with a chapter on "pre-history," which extends from the paleolithic to the moment of Russian arrival in the late sixteenth, early seventeenth centuries. *2 The goal is usually to enable the reader to understand what "human material" the Russians found and what "progress" was then achieved. Inherent in the narratives -- however sympathetic they may or may not be to the native peoples -- are assumptions about the historical advance deriving from the Russian arrival and socio-economic transformation. In short, the narratives are involved in legitimating Russia's conquest without any notion of alternatives. Of course, history can also be used to show that what seems natural did not exist forever but came into being; to reveal that there were other modes of existence, which were either pushed aside or folded into what then came to seem irreversible.
    [Show full text]
  • Tectonic Evolution of the SE West Siberian Basin (Russia): Evidence from Apatite Fission Track Thermochronology of Its Exposed Crystalline Basement
    minerals Article Tectonic Evolution of the SE West Siberian Basin (Russia): Evidence from Apatite Fission Track Thermochronology of Its Exposed Crystalline Basement Evgeny V. Vetrov 1,*, Johan De Grave 2, Natalia I. Vetrova 1, Fedor I. Zhimulev 1 , Simon Nachtergaele 2 , Gerben Van Ranst 3 and Polina I. Mikhailova 4 1 Sobolev Institute of Geology and Mineralogy SB RAS, 630082 Novosibirsk, Russia; [email protected] (N.I.V.); [email protected] (F.I.Z.) 2 Department of Geology, Mineralogy and Petrology Research Unit, Ghent University, 9000 Ghent, Belgium; [email protected] (J.D.G.); [email protected] (S.N.) 3 Environment Unit, Antea Group Belgium, 2600 Antwerpen, Belgium; [email protected] 4 Siberian Research Institute of Geology, Geophysics and Mineral Resources, 630091 Novosibirsk, Russia; [email protected] * Correspondence: [email protected] Abstract: The West Siberian Basin (WSB) is one of the largest intracratonic Meso-Cenozoic basins in the world. Its evolution has been studied over the recent decades; however, some fundamental ques- tions regarding the tectonic evolution of the WSB remain unresolved or unconfirmed by analytical data. A complete understanding of the evolution of the WSB during the Mesozoic and Cenozoic eras Citation: Vetrov, E.V.; De Grave, J.; requires insights into the cooling history of the basement rocks as determined by low-temperature Vetrova, N.I.; Zhimulev, F.I.; thermochronometry. We presented an apatite fission track (AFT) thermochronology study on the Nachtergaele, S.; Van Ranst, G.; Mikhailova, P.I. Tectonic Evolution of exposed parts of the WSB basement in order to distinguish tectonic activation episodes in an absolute the SE West Siberian Basin (Russia): timeframe.
    [Show full text]
  • Hymenoptera, Apidae: Bombus Latreille, 1802) of the Republic of Khakassia, Eastern Siberia
    Number 261: 1-12 ISSN 1026-051X April 2013 hppt/ urn:lsid:zoobank.org:pub: 170D14D4-8B66-4DFD-B288-91BD3AA7ED8D CONTRIBUTION TO THE FAUNA OF BUMBLE BEES (HYMENOPTERA, APIDAE: BOMBUS LATREILLE, 1802) OF THE REPUBLIC OF KHAKASSIA, EASTERN SIBERIA A. N. Kupianskaya, M. Yu. Proshchalykin, A. S. Lelej Institute of Biology and Soil Science, Far Eastern Branch of the Russian Academy of Sciences, Vladivostok 690022, Russia. E-mail: [email protected] An annotated list of nineteen species of bumble bees collected in the Republic of Khakassia in 2012 is given. The list accounts 32 species including one doubtful species. Eleven species: Bombus barbutellus (Kirby), B. confusus Schenck, B. filchnerae Vogt, B. hortorum (Linnaeus), B. patagiatus Nylander, B. pseudobai- calensis Vogt, B. ruderarius (Müller), B. sibiricus (Fabricius), B. subterraneus (Linnaeus), B. sylvarum (Linnaeus) and B. veteranus (Fabricius) are newly recorded from Khakassia. Patterns of bumble bees diversity in the Khakassia and Siberia are discussed. KEY WORDS: Apoidea, Apiformes, Palaearctic region, biodiversity, new records. А. Н. Купянская, М. Ю. Прощалыкин, А. С. Лелей. К фауне шмелей (Hymenoptera, Apidae: Bombus Latreille, 1802) Республики Хакасия, Восточная Сибирь // Дальневосточный энтомолог. 2013. № 261. C. 1-12. Приведен аннотированный список 19 видов шмелей, собранных в Респуб- лике Хакасия в 2012 г. Список включает 32 вида, включая один сомнительный. Одиннадцать видов: Bombus barbutellus (Kirby), B. confusus Schenck, B. filchnerae 1 Vogt, B. hortorum (Linnaeus), B. patagiatus Nylander, B. pseudobaicalensis Vogt, B. ruderarius (Müller), B. sibiricus (Fabricius), B. subterraneus (Linnaeus), B. sylvarum (Linnaeus) и B. veteranus (Fabricius) впервые указываются для фауны Хакасии. Обсуждаются особенности разнообразия шмелей в Хакасии и Си- бири.
    [Show full text]
  • In the South of Western Siberia
    Pak. J. Bot., 49(3): 1057-1061, 2017. A STUDY OF THE ENVIRONMENTAL-CENOTIC CONFINEDNESS OF ATRAGENE SPECIOSA WEINM. (RANUNCULACEAE) IN THE SOUTH OF WESTERN SIBERIA AN NEKRATOVA* National Research Tomsk State University, Tomsk, Lenina ave., 36. *Corresponding author email:[email protected] Abstract Atragene speciosa Weinm.of the family Ranunculaceae is an adventitious species. It has reserves of raw materials of the third category, i.e., it is a rare and non-exploited plant in KuznetskyAlatau and in Tomsk Region, Russia. In those areas of Western Siberia in plant communities with Atragene speciose Weinm. there are 124 species, of which 82 species grow in KuznetskyAlatau, 75 species in Tomsk Region, and 29 species grow together with Atragene speciosa Weinm. In KuznetskyAlatau and Tomsk egion at the same time. Key words: Atragene speciosa, Western Siberia, Environmental-cenotic confinedness. Introduction taiga, II - Kuznetsk-Altai high-mountain, III – North Kuznetsk-Altai dark-light coniferous, IV – East Kuznetsk- Currently, the expansion of the range of medicinal Altai midland dark-light coniferous, V - Balyksinsky products through the introduction of new drugs of mountain taiga, VI - Batenevsky lowland forest-steppe nootropic action is one of the priorities in the world of (Maskaev, 1976; Nekratova, 2005). Geo-botanical medicine (Deeb et al., 2013; Ikram et al., 2015; Shilova et descriptions of Atragene speciosa Weinm. are given al., 2013; Shinwari & Qaiser, 2011). The chemical mainly for the East Kuznetsk-Altai midland dark-light properties of the aerial part of Atragene speciosa Weinm. coniferous district. In Tomsk Region geo-botanical were studied at the E.D. Goldberg SB RAMS Institute of descriptions are given for Tomsk and Molchanovskiy Pharmacology; the scientists established the expressive districts.
    [Show full text]
  • S I Mikhailova Maxin.Pmd
    BIOSCIENCES BIOTECHNOLOGY RESEARCH ASIA, December 2015. Vol. 12(3), 2045-2052 Malva verticillata L. and Vicia hirsuta (L.) S.F. Gray - invasive Species of Siberia (Overview) S.I. Mikhailova and A.L. Ebel National Research Tomsk State University, 36 Lenina Avenue, Tomsk, 634050, Russia. DOI: http://dx.doi.org/10.13005/bbra/1872 (Received: 16 September 2015; accepted: 06 November 2015) The article provides an overview of information on the two invasive species of Siberia that are weeds of crops - Malva verticillata L. and Vicia hirsuta (L.) S.F. Gray. It provides information on the distribution of species, morphology, biological and ecological characteristics. Active ability of Vicia hirsuta to spread with the seed of oil plants and honey plants was revealed. The possible consequences of the introduction in natural plant communities are shown. The possibility of the practical use of these species as fodder, food and medicinal plants is considered. Key words: invasive species, Malva verticillata, Vicia hirsuta, Siberia, distribution, speirochoria. Currently, weed-field (segetal) plant (D’Antonio, Meyerson, 2002; Richardson et al., species are an important component of agrocoenosis 2007). It is known that invasion of the invasive in Russia. Species composition and abundance of species leads to a reduction of biological diversity weeds in agricultural crops largely determine the (Hejda, Pysek, 2006; Winter et al., 2009). However, efficiency and quality of the crop production. the invasion of “harmful” alien species caused Weeds are an annual permanent factor that reduces great damage not only to natural ecosystems, but the yield of economically valuable products, such also to the economies of developed and developing as cereals - by 20-25%, and vegetables - by 50%.
    [Show full text]
  • Kemerovo Region Investment Passport 1 Kemerovo Region Investment Passport
    Kemerovo Region State public institutions "Agency for Investments Promotion and Protection" Kemerovo region investment passport 1 Kemerovo region investment passport KEMEROVO REGION RUSSIAN FEDERATION 2 Dear investors! I greet you in our hospitable region! Its task is to promote the potential of Kuzbass at interre- Kuzbass is the largest coal and metallurgical center gional and international levels, attract investment and in Russia and one of the main industrial regions of the support investment projects on the principle of "one win- country. Currently we create conditions for Kemerovo dow". What is important, the agency provides its servic- region to become also a territory of developed agricul- es free of charge. With the assistance of the agency the ture, fascinating year-round tourism and a scientific and Kuzbass Investors' Club was created. It is a platform for cultural center. exchanging information between entrepreneurs, inves- We set ourselves an ambitious goal to make Kuzbass tors and authorities. the region No. 1 in Siberia. Providing a favorable investment climate and sup- First of all concerning quality of people's lives. porting projects are the permanent priorities of our in- Our region has a great potential and a set of com- vestment policy. This is reflected in the strategy of at- petitive advantages for conducting economic activity. tracting investments in Kemerovo region until 2030. Three territories of advanced social and economic To maximize the region economic potential use, we development (TASED) have been created and are actively began a work on a large-scale program for region devel- operating on the territory of three Kuzbass mono cities.
    [Show full text]
  • Precipitation Reconstruction for the Khakassia Region, Siberia, from Tree Rings
    HOL0010.1177/0959683617729450The HoloceneKostyakova et al. 729450research-article2017 Research paper The Holocene 2018, Vol. 28(3) 377 –385 Precipitation reconstruction for the © The Author(s) 2017 Reprints and permissions: sagepub.co.uk/journalsPermissions.nav Khakassia region, Siberia, from tree rings DOI:https://doi.org/10.1177/0959683617729450 10.1177/0959683617729450 journals.sagepub.com/home/hol Tatiana V Kostyakova,1 Ramzi Touchan,2 Elena A Babushkina1 and Liliana V Belokopytova1 Abstract A nested July–June precipitation reconstruction for the period AD 1777–2012 was developed from multi-century tree-ring records of Pinus sylvestris L. (Scots pine) for the Republic of Khakassia in Siberia, Russia. Calibration and verification statistics for the period 1948–2012 show a high level of skill and account for a significant portion of the observed variance (>50%) irrespective of which period is used to develop or verify the regression model. Split- sample validation supports our use of a reconstruction model based on the full period of reliable observational data (1948–2012). Thresholds (25th and 75th percentiles) based on the empirical cumulative distribution of 1948–2012 observed precipitation were used to delineate dry years and wet years of the long-term reconstruction. The longest reconstructed dry period, defined as consecutive years with less than 25th percentile of observed July–June precipitation, was 3 years (1861–1863). There was no significant difference in the number dry and wet periods during the 236 years of the reconstructed precipitation. Maps of geopotential height anomalies indicate that dry years differ from wet years primarily in the location of an anomalous 500-mb ridge approximately over the study area.
    [Show full text]
  • Tectonic History of the Kolyvan-Tomsk Folded Zone (KTFZ), Russia: Insight from Zircon U/Pb Geochronology and Nd Isotopes
    Tectonic history of the Kolyvan-Tomsk folded zone (KTFZ), Russia: Insight from zircon U/Pb geochronology and Nd isotopes Item Type Article Authors Zhimulev, Fedor I.; Gillespie, Jack; Glorie, Stijn; Jepson, Gilby; Vetrov, Evgeny V.; De Grave, Johan Citation Zhimulev, FI, Gillespie, J, Glorie, S, Jepson, G, Vetrov, EV, De Grave, J. Tectonic history of the Kolyvan–Tomsk folded zone (KTFZ), Russia: Insight from zircon U/Pb geochronology and Nd isotopes. Geological Journal. 2020; 55: 1913– 1930. https:// doi.org/10.1002/gj.3679 DOI 10.1002/gj.3679 Publisher WILEY Journal GEOLOGICAL JOURNAL Rights © 2019 John Wiley & Sons, Ltd. Download date 27/09/2021 15:01:23 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final accepted manuscript Link to Item http://hdl.handle.net/10150/641031 1 Tectonic history of the Kolyvan-Tomsk folded zone (KTFZ), Russia: insight from zircon 2 U/Pb geochronology and Nd isotopes 3 Fedor I. Zhimuleva*, Jack Gillespieb, Stijn Glorieb, Gilby Jepsonb, c, Evgeny V. Vetrova, d, 4 Johan De Gravee 5 a Sobolev Institute of Geology and Mineralogy Siberian Вrаnch Russian Academy of 6 Sciences, Novosibirsk 630090 Koptuga ave. 3, Russia 7 b Tectonics, Resources and Exploration (TraX), Department of Earth Sciences, University of 8 Adelaide, Adelaide, Australia 9 c Department of Geosciences, University of Arizona, Tucson, AZ, USA 10 11 d Siberian Research Institute of Geology, Geophysics and Mineral Resources, Novosibirsk, 12 630099 Krasniy ave. 35, Russia. 13 e Department of Geology, Ghent University, Krijgslaan 281.S8, WE13, 9000 Gent, Belgium 14 15 * Corresponding author: 16 Sobolev Institute of Geology and Mineralogy Siberian Вrаnch Russian Academy of Sciences, 17 Novosibirsk, Russia 18 [email protected], [email protected] 19 20 21 Abstract 22 The Kolyvan-Tomsk folded zone (KTFZ) represents part of the Central Asian Orogenic Belt 23 (CAOB).
    [Show full text]
  • Assessment Report: Climate Change and Its Impact on Ecosystems, Population and Economy of the Russian Portion of the Altai-Sayan Ecoregion
    UNDP/GEF/ICI Project BIodivErsIty CoNsErvatIoN in thE RussIaN PortIoN oF thE altaI-sayaN ECoregioN Assessment Report: Climate change and its impact on ecosystems, population and economy of the Russian portion of the Altai-Sayan Ecoregion WWF russia Moscow • 2011 Authors: T. A. Blyakharchuk, D.Sc. (Biology), Institute of Monitoring of Climatic and Ecological Systems, Siberian Branch CONTENTS of the Russian Academy of Sciences (RAS) (Sub-section 5.1) I. V. Gerasimchuk, Ph.D. (Economics), Cyprus International Institute of Management (Section 6) 5 G. V. Gruza, D.Sc. (Physics and Mathematics), Prof., Institute of Global Climate and Ecology under RAS and the Introduction Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet) (Section 2) I. E. Kamennova, WWF Russia (Section 4) 1. overview of the altai-sayan Ecoregion 12 A. O. Kokorin, Ph.D. (Physics and Mathematics), WWF Russia (Section 4) Ye. I. Parfenova, Ph.D. (Biology), Institute of Forest, RAS Siberian Branch (Subsections 3.1 & 5.1) 2. Climate Change in the russian Portion of the altai-sayan Ecoregion E. Ya. Rankova, D.Sc. (Physics and Mathematics), RAS&Roshydromet Institute of Global Climate and Ecology (E.ya. rankova and G.v. Gruza) 14 (Section 2) 2.1. Climate, Climate Change and Climatic variability (Fundamental Definitions) 14 V. A. Semenov, D.Sc. (Geography), Prof., All Russian Research Institute of Hydrometeorological Information – World Data Center under Roshydromet (Subsections 3.2 & 5.2) 2.2. Climate Change observed During recent Decades 15 N. M. Tchebakova, D.Sc. (Biology), Institute of Forest, RAS Siberian Branch (Subsections 3.1 & 5.1) 2.2.1.
    [Show full text]