班公湖-怒江缝合带西段沙木罗组泥质岩地球化学特征及意义
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摘要
沙木罗组分布于班公湖-怒江缝合带内部,其沉积背景、源区性质与班-怒特提斯洋的演化息息相关。为了研究班怒带西段沙木罗组泥质岩的物源特征,探讨沉积盆地的构造背景和班-怒特提斯洋的俯冲消减时限,对泥质岩开展了全岩主量元素、微量元素地球化学的研究。地球化学组成特征显示,泥质岩的ICV、CIA、Al2O3/TiO_2、Th/Sc、Rb/Cs、(Gd/Yb)N、La、Ce、∑REE、La/Yb、(La/Yb)N、Eu/Eu*N和LREE/HREE均值分别为0. 80、72、21、0. 88、13. 5、1.58、42. 47×10-6、84. 81×10-6、200. 02×10-6、14. 22、9. 61、0. 65和9. 04,具有中等的Th、U、Hf含量(分别为16. 34×10-6、2. 85×10-6和4. 81×10-6)和Th/U、La/Th值(分别为5. 78和2. 61)。泥质岩的K2O/Na2O-SiO2、La-Th-Sc、ThCo-Zr/10、Th-Sc-Zr/10、TiO_2-Zr、Co/Y-Ti/Zr、La-Th-Sc、Th-Sc、La/Sc-Co/Th、REE-La/Yb、A-CN-K等关系图解具较好的指示意义,稀土元素特征亦具有一定的规律性。上述地球化学特征表明,泥质岩为成熟的泥质岩,源区矿物组成以斜长石、碱性长石为主,源区母岩主要为后太古宙花岗闪长岩、花岗岩、安山岩等中酸性岩浆岩和碎屑岩。泥质岩源区母岩经历了中等程度的化学风化作用,沉积物沉积时气候较温暖、湿润。不同层位的泥质岩地球化学特征指示了班怒带西段沙木罗组沉积于活动大陆边缘的构造背景,从剖面下部到上部可能反映了板块俯冲加剧、岩浆活动加强的地质过程,至少在141 Ma左右班-怒特提斯洋西段正在向北俯冲消减。
The Shamuluo Formation is distributed in Bangong Co-Nujiang suture zone, and its sedimentary background and source characteristic were closely linked with the evolution of Bangong Co-Nujiang Tethys Ocean. In order to discuss sediment provenance, weathering, tectonic setting of sedimentary basin and subduction of Bangong Co-Nujiang Tethys Ocean, the authors made a systematic analysis of petrology and geochemistry of Shamuluo Formation argillaceous rocks in the western part of the Bangong Co-Nujiang suture zone. The mean values of ICV,CIA, Al2O3/TiO_2, Th/Sc, Rb/Cs,(Gd/Yb)N, La, Ce, ∑REE, La/Yb,(La/Yb)N, Eu/Eu*N, LREE/HREE are 0. 80, 72, 21, 0. 88, 13. 5, 1. 58, 42. 47 × 10-6, 84. 81 × 10-6, 200. 02 × 10-6, 14. 22, 9. 61, 0. 65 and9. 04 respectively, while the mean values of Th, U, Hf, Th/U, La/Th are 16. 34 × 10-6, 2. 85 × 10-6, 4. 81 ×10-6, 5. 78 and 2. 61 respectively. The diagrams of K2O/Na2O-SiO2, La-Th-Sc, Th-Co-Zr/10, Th-Sc-Zr/10,TiO_2-Zr, Co/Y-Ti/Zr, La-Th-Sc, Th-Sc, La/Sc-Co/Th, REE-La/Yb, A-CN-K and REEs also show certain regularity. The argillaceous rocks are mature and the source rock are granodiorite, granite, andesite and sedimentary clastic rock which have much plagioclase and alkali feldspar. The source region of argillaceous rocks has suffered from medium degree of chemical weathering, suggesting a warm and moist climate. The geochemical characteristics of argillaceous rocks indicate that argillaceous rocks tended to occur in active continental margin setting, where its tectonic activity became intensified from the bottom to the top. These results provide sedimentary geochemical evidence for the evolution of Bangong Co-Nujiang Tethys Ocean, which indicates that Bangong Co-Nujiang Tethys Ocean experienced northward subduction about 141 million years ago.
The Shamuluo Formation is distributed in Bangong Co-Nujiang suture zone, and its sedimentary background and source characteristic were closely linked with the evolution of Bangong Co-Nujiang Tethys Ocean. In order to discuss sediment provenance, weathering, tectonic setting of sedimentary basin and subduction of Bangong Co-Nujiang Tethys Ocean, the authors made a systematic analysis of petrology and geochemistry of Shamuluo Formation argillaceous rocks in the western part of the Bangong Co-Nujiang suture zone. The mean values of ICV,CIA, Al2O3/TiO_2, Th/Sc, Rb/Cs,(Gd/Yb)N, La, Ce, ∑REE, La/Yb,(La/Yb)N, Eu/Eu*N, LREE/HREE are 0. 80, 72, 21, 0. 88, 13. 5, 1. 58, 42. 47 × 10-6, 84. 81 × 10-6, 200. 02 × 10-6, 14. 22, 9. 61, 0. 65 and9. 04 respectively, while the mean values of Th, U, Hf, Th/U, La/Th are 16. 34 × 10-6, 2. 85 × 10-6, 4. 81 ×10-6, 5. 78 and 2. 61 respectively. The diagrams of K2O/Na2O-SiO2, La-Th-Sc, Th-Co-Zr/10, Th-Sc-Zr/10,TiO_2-Zr, Co/Y-Ti/Zr, La-Th-Sc, Th-Sc, La/Sc-Co/Th, REE-La/Yb, A-CN-K and REEs also show certain regularity. The argillaceous rocks are mature and the source rock are granodiorite, granite, andesite and sedimentary clastic rock which have much plagioclase and alkali feldspar. The source region of argillaceous rocks has suffered from medium degree of chemical weathering, suggesting a warm and moist climate. The geochemical characteristics of argillaceous rocks indicate that argillaceous rocks tended to occur in active continental margin setting, where its tectonic activity became intensified from the bottom to the top. These results provide sedimentary geochemical evidence for the evolution of Bangong Co-Nujiang Tethys Ocean, which indicates that Bangong Co-Nujiang Tethys Ocean experienced northward subduction about 141 million years ago.
引文
Allègre C J and Minster J F.1978.Quantitative models of trace element behavior in magmatic processes[J].Earth&Planetary Science Letters,38(1):1~25.
Banerjee D M and Bhattacharya P.1994.Petrology and geochemistry of greywackes from the Aravalli Supergroup,Rajasthan,India and the tectonic evolution of a Proterozoic sedimentary basin[J].Precambrian Research,67(1~2):11~35.
Bhat M I and Ghosh S K.2001.Geochemistry of the 2.51 Ga old Rampur group pelites,western Himalayas:Implications for their provenance and weathering[J].Precambrian Research,108(1~2):1~16.
Bhatia M R.1985.Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks:Provenance and tectonic control[J].Sedimentary Geology,45(1):97~113.
Bhatia M R and Crook K A W.1986.Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J].Contributions to Mineralogy and Petrology,92(2):181~193.
Bhatia M R and Taylor S R.1981.Trace-element geochemistry and sedimentary provinces:A study from the Tasman Geosyncline,Australia[J].Chemical Geology,33(1):115~125.
Chang C F,Chen N,Coward M P,et al.1986.Preliminary conclusions of the Royal Society and Academia Sinica 1985 geotraverse of Tibet[J].Nature,323:501~507.
Chen Guorong,Liu Hongfei,Jiang Guangwu,et al.2004.Discovery of the Shamuluo Formation in the central segment of the Bangong Co-Nujiang River suture zone,Tibet[J].Geological Bulletin of China,23(2):193~194(in Chinese with English abstract).
Chi Qinghua and Yan Mingcai.2007.Handbook of Elemental Abundance for Applied Geochemistry[M].Beijing:Geological Publishing House,148(in Chinese with English abstract).
Condie K C.1993.Chemical composition and evolution of the upper continental crust:Contrasting results from surface samples and shales[J].Chemical Geology,104(1~4):1~37.
Cox R and Lowe D R.1995.A conceptual review of regional-scale controls on the composition of clastic sediment and the co-evolution of continental blocks and their sedimentary cover[J].Journal of Sedimentary Research Section A-Sedimentary Petrology and Processes,65(1):1~12.
Cox R,Lowe D R and Cullers R L.1995.The influence of sediment recycling and basement composition on evolution of mudrock chemistry in the southwestern United States[J].Geochimica et Cosmochimica Acta,59(14):2 919~2 940.
Cullers R L.1994.The controls on the major and trace element variation of shales,siltstones,and sandstones of Pennsylvanian-Permian age from uplifted continental blocks in Colorado to platform sediment in Kansas,USA[J].Geochimica et Cosmochimica Acta,58(22):4 955~4 972.
Cullers R L and Podkovyrov V N.2000.Geochemistry of the Mesoproterozoic Lakhanda shales in southeastern Yakutia,Russia:implications for mineralogical and provenance control,and recycling[J].Precambrian Research,104(1):77~93.
Du Dedao,Qu Xiaoming,Wang Genhou,et al.2011.Bidirectional subduction of the middle Tethys oceanic basin in the west segment of Bangonghu-Nujiang Suture,Tibet:Evidence from Zircon U-Pb LA-ICPMS dating and petrogeochemistry of arc granites[J].Acta Petrologica Sinica,27(7):1 993~2 002(in Chinese with English abstract).
Fedo C M,Nesbitt H W and Young G M.1995.Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols,with implications for paleoweathering conditions and provenance[J].Geology,23(10):921~924.
Fedo C M,Young G M,Nesbitt H W,et al.1997.Potassic and sodic metasomatism in the Southern Province of the Canadian Shield:Evidence from the Paleoproterozoic Serpent Formation,Huronian Supergroup,Canada[J].Precambrian Research,84(1~2):17~36.
Feng Lianjun,Chu Xuelei,Zhang Qirui,et al.2003.CIA(chemical index of alteration)and its applications in the Neoproterozoic clastic rocks[J].Earth Science Frontiers(China University of Geosciences,Beijing),10(4):539~544(in Chinese with English abstract).
Haskin M A and Haskin L A.1966.Rare Earths in European Shales:ARedetermination[J].Science,154(3 748):507~509.
Hayashi K,Fujisawa H,Holland H D,et al.1997.Geochemistry of similar to 1.9 Ga sedimentary rocks from northeastern Labrador,Canada[J].Geochimica et Cosmochimica Acta,61(19):4 115~4 137.
Huang Qishuai,Shi Rendeng,Ding Binghua,et al.2012.Re-Os isotopic evidence of MOR-type ophiolite from the Bangong Co for the opening of Bangong-Nujiang Tethys Ocean[J].Acta Petrologica et Mineralogica,31(4):465~478(in Chinese with English abstract).
Ishiga H and Dozen K.1997.Geochemical indications of provenance change as recorded in Miocene shales:opening of the Japan Sea,San'in region,southwest Japan[J].Marine Geology,144(1):211~228.
Kapp P,Murphy M A,Yin A,et al.2003.Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet[J].Tectonics,22(4):253.
Liang Sang,Zhou Tao,Li Dewei,et al.2017.Timing of southward subduction of Meso-tethys in Bangong Lake:Constraints from supra-subduction zone(SSZ)-type gabbro[J].Geotectonica et Metallogenia,41(5):989~1 000(in Chinese with English abstract).
Liu D,Huang Q,Fan S,et al.2014.Subduction of the Bangong-Nujiang Ocean:Constraints from granites in the Bangong Co area,Tibet[J].Geological Journal,49(2):188~206.
Liu W,Xia B,Zhong Y,et al.2014.Age and composition of the Rebang Co and Julu ophiolites,central Tibet:Implications for the evolution of the Bangong Meso-Tethys[J].International Geology Review,56(4):430~447.
Liu Z F,Colin C,Huang W,et al.2007.Climatic and tectonic controls on weathering in south China and Indochina Peninsula:Clay mineralogical and geochemical investigations from the Pearl,Red,and Mekong drainage basins[J].Geochemistry,Geophysics,Geosystems,8(5):Q5005.
Mclennan S M.1993.Weathering and global denudation[J].Journal of Geology,101(2):295~303.
Mc Lennan S M,Hemming S R,Mc Daniel D K,et al.1993.Geochemical approaches to sedimentation,provenance,and tectonics[J].Geological Society of America Special Papers,284:21~40.
Mc Lennan S M,Hemming S R,Taylor S R,et al.1995.Early Proterozoic crustal evolution:Geochemical and Nd-Pb isotopic evidence from metasedimentary rocks,southwestern North America[J].Geochimica et Cosmochimica Acta,59(6):1 153~1 177.
Murray R W,Buchholtz Ten Brink M R,Jones D L,et al.1990.Rare earth elements as indicators of different marine depositional environments in chert and shale[J].Geology,18(3):268~271.
Naqvi S M,Sawkar R H,Rao D,et al.1988.Geology,geochemistry and tectonic setting of Archaean greywackes from Karnataka Nucleus,India[J].Precambrian Research,39(3):193~216.
Nesbitt H W and Young G M.1982.Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J].Nature,299(5885):715~717.
Nesbitt H W and Young G M.1989.Formation and diagenesis of weathering profiles[J].Journal of Geology,97(2):129~147.
Nesbitt H W and Young G M.1984.Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J].Geochimica et Cosmochimica Acta,48(7):1 523~1 534.
Nesbitt H W,Young G M,Mc Lennan S M,et al.1996.Effects of chemical weathering and sorting on the petrogenesis of siliciclastic sediments,with implications for provenance studies[J].Journal of Geology,104(5):525~542.
Pan Guitang,Mo Xuanxue,Hou Zengqian,et al.2006.Spatial-temporal Framework of the Gangdese Orogenic Belt and Its Evolution[J].Acta Petrologica Sinica,22(3):521~533(in Chinese with English abstract).
Passchier S and Krissek L A.2008.Oligocene-Miocene Antarctic continental weathering record and paleoclimatic implications,Cape Roberts drilling project,Ross Seal,Antarctica[J].Palaeogeography,Palaeoclimatology,Palaeoecology,260(1~2):30~40.
Plank T and Langmuir C H.1998.The chemical composition of subducting sediment and its consequences for the crust and mantle[J].Chemical Geology,145(3~4):325~394.
Qiu Ruizhao,Zhou Shu,Deng Jingfu,et al.2004.Dating of gabbro in the Shemalagou ophiolite in the western segment of the Bangong CoNujiang ophiolite belt,Tibet:With a discussion of the age of the Bangong Co-Nujiang ophiolite belt[J].Geology in China,31(3):262~268(in Chinese with English abstract).
Qu Xiaoming,Wang Ruijiang,Xin Hongbo,et al.2009.Geochronology and geochemistry of igneous along the Bangong Lake rocks related to the subduction of the Tethys oceanic plate arc zone,the western Tibetan Plateau[J].Geochimica,38(6):523~535(in Chinese with English abstract).
Qu Xiaoming,Xin Hongbo,Zhao Yuanyi,et al.2010.Opening time of Bangong Lake Middle Tethys Oceanic Basin of the Tibet Plateau:Constraints from petro-geochemistry and zircon U-Pb LAICPMS dating of mafic ophiolites[J].Earth Science Frontiers(China University of Geosciences,Beijing),17(3):53~63(in Chinese with English abstract).
Roser B P and Korsch R J.1986.Determination of tectonic setting of sandstone-mudstone suits using SiO2content and K2O/Na2O ratio[J].Journal of Geology,94(5):635~650.
Savoy L E,Stevenson R K and Mountjoy E W.2000.Provenance of Upper Devonian-Lower Carboniferous miogeoclinal strata,southeastern Canadian Cordillera:Link between tectonics and sedimentation[J].Journal of Sedimentary Research,70(1A):181~193.
Scheffler K,Buehmann D and Schwark L.2006.Analysis of Late Palaeozoic glacial to postglacial sedimentary successions in South Africa by geochemical proxies-Response to climate evolution and sedimentary environment[J].Palaeogeography,Palaeoclimatology,Palaeoecology,240(1~2):184~203.
Shao Lei,Li Xianhua,Wei Gangjian,et al.2001.The slope of the South China Sea material sources of the deposit[J].Science in China(Series D),31(10):828~833(in Chinese with English abstract).
Shi Rendeng.2007.The geochronology of SSZ-type ophiolites:Constraints on the evolution time of the Bangong Lake-Nujiang ocean basin[J].Chinese Science Bulletin,52(2):223~227(in Chinese with English abstract).
Sreenivas B and Srinivasan R.1994.Identification of paleosols in the Precambrian metapelitic assemblages of peninsular India major element geochemical approach[J].Current Science,67(2):89~94.
Taylor S R and Mc Lennan S M.1985.The Continental Crust:Its Composition and Evolution[M].Oxford:Blackwell Scientific Publications,312.
Totten M W,Hanan M A and Weaver B L.2000.Beyond whole-rock geochemistry of shales:The importance of assessing mineralogic controls for revealing tectonic discriminants of multiple sediment sources for the Ouachita Mountain flysch deposits[J].Geological Society of A-merica Bulletin,112(7):1 012~1 022.
Wang W,Aitchison J C,Lo C,et al.2008.Geochemistry and geochronology of the amphibolite blocks in ophiolitic mélanges along BangongNujiang suture,central Tibet[J].Journal of Asian Earth Sciences,33(1~2):122~138.
Wang Xibin.1987.Lithospheric Evolution of Himalayan:Tibet Ophiolites[M].Beijing:Geological Publishing House,336(in Chinese with English abstract).
Wani H and Mondal M E A.2011.Evaluation of provenance,tectonic setting,and paleoredox conditions of the Mesoproterozoic-Neoproterozoic basins of the Bastar craton,Central Indian Shield:Using petrography of sandstones and geochemistry of shales[J].Lithosphere,3(2):143~154.
Xie Bingjing,Cheng Jie and Huang Chuanguan.2010.The found and the significance for the west area of Samut Luo Group in the Bangong Lake-Nu River suture[J].Journal of East China Institute of Technology,33(2):159~164(in Chinese with English abstract).
Xu Wenli,Zheng Rongcai,Yan Xue,et al.2014.Trace and rare earth element geochemistry of the Early Paleozoic black shales in the Lower Yangtze area and its geological significances[J].Journal of Jilin University(Earth Science Edition),44(4):1 108~1 122(in Chinese with English abstract).
Yang S Y,Yim W W S and Huang G Q.2008.Geochemical composition of inner shelf quaternary sediments in the northern South China Sea with implications for provenance discrimination and paleoenvironmental reconstruction[J].Global and Planetary Change,60(3~4):207~221.
Yin A and Harrison T M.2000.Geologic evolution of the Himalayan-Tibetan orogen[J].Annual Review of Earth and Planetary Sciences,28:211~280.
Young G M and Nesbitt H W.1999.Paleoclimatology and provenance of the glaciogenic Gowganda Formation(Paleoproterozoic),Ontario,Canada:A chemostratigraphic approach[J].Geological Society of America Bulletin,111(2):264~274.
Zhang H.1988.The structure of the 1985 Tibet geotraverse,Lhasa to Golmud:Appendix,structures and fabrics in the Kunlun Shan:Evidence for Mid-Palaeozoic(Pre-Upper Devonian)deformation[J].Philosophical Transactions of The Royal Society A Mathematical Physical and Engineering Sciences,327(1 594):334~336.
Zhang Jingliang and Zhang Xin.2006.The Element geochemical features of ancient oceanic sedimentary environments in the Silurian period in the Tarim Basin[J].Periodical of Ocean University of China,36(2):200~208(in Chinese with English abstract).
Zhang K,Xia B,Wang G,et al.2004.Early Cretaceous stratigraphy,depositional environments,sandstone provenance,and tectonic setting of central Tibet,western China[J].Geological Society of America Bulletin,116(9):1 202.
Zhang Yuxiu.2007.Tectonic Evoiution of the Middle-western BangongNujiang Suture,Tibet(PHD Dissertation)[D].Guangzhou:Graduate School of the Chinese Academy of Sciences(in Chinese with English abstract).
Zhao Zhenhua.2016.The Elements of the Trace Element Geochemistry[M].Beijing:Science Press,534(in Chinese with English abstract).
Zhou Tao,Chen Chao,Liang Sang,et al.2014.Zircon U-Pb geochronology and geochemical characteristics of volcanic rocks in the ophiolite melange at the Bangong Lake,Tibet[J].Geotectonica et Metallogenia,38(1):157~167(in Chinese with English abstract).
Zhu D,Zhao Z,Niu Y,et al.2013.The origin and pre-Cenozoic evolution of the Tibetan Plateau[J].Gondwana Research,23(4):1 429~1 454.
陈国荣,刘鸿飞,蒋光武,等.2004.西藏班公湖-怒江结合带中段沙木罗组的发现[J].地质通报,23(2):193~194.
迟清华,鄢明才.2007.应用地球化学元素丰度数据手册[M].北京:地质出版社,148.
杜德道,曲晓明,王根厚,等.2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据[J].岩石学报,27(7):1 993~2 002.
冯连君,储雪蕾,张启锐,等.2003.化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用[J].地学前缘,10(4):539~544.
黄启帅,史仁灯,丁炳华,等.2012.班公湖MOR型蛇绿岩Re-Os同位素特征对班公湖-怒江特提斯洋裂解时间的制约[J].岩石矿物学杂志,31(4):465~478.
梁桑,周涛,李德威,等.2017.班公湖中特提斯洋向南俯冲的时限:来自SSZ型辉长岩的制约[J].大地构造与成矿学,41(5):989~1 000.
潘桂棠,莫宣学,侯增谦,等.2006.冈底斯造山带的时空结构及演化[J].岩石学报,22(3):521~533.
邱瑞照,周肃,邓晋福,等.2004.西藏班公湖-怒江西段舍马拉沟蛇绿岩中辉长岩年龄测定---兼论班公湖-怒江蛇绿岩带形成时代[J].中国地质,31(3):262~268.
曲晓明,王瑞江,辛洪波,等.2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学[J].地球化学,38(6):523~535.
曲晓明,辛洪波,赵元艺,等.2010.西藏班公湖中特提斯洋盆的打开时间:镁铁质蛇绿岩地球化学与锆石U-Pb LA-ICP-MS定年结果[J].地学前缘,17(3):53~63.
邵磊,李献华,韦刚健,等.2001.南海陆坡高速堆积体的物质来源[J].中国科学(D辑:地球科学),31(10):828~833.
史仁灯.2007.班公湖SSZ型蛇绿岩年龄对班-怒洋时限的制约[J].科学通报,52(2):223~227.
王希斌.1987.喜马拉雅岩石圈构造演化---西藏蛇绿岩[J].北京:地质出版社,336.
谢冰晶,程捷,黄传冠.2010.班公湖怒江结合带西段沙木罗组的发现及意义[J].东华理工大学学报(自然科学版),33(2):159~164.
徐文礼,郑荣才,颜雪,等.2014.下扬子地区早古生代黑色岩系地球化学特征及其地质意义[J].吉林大学学报(地球科学版),44(4):1 108~1 122.
张玉修.2007.班公湖-怒江缝合带中西段构造演化[D].广州:广州地球化学研究所.
张金亮,张鑫.2006.塔里木盆地志留系古海洋沉积环境的元素地球化学特征[J].中国海洋大学学报(自然科学版),36(2):200~208.
赵振华.2016.微量元素地球化学原理[M].北京:科学出版社,534.
周涛,陈超,梁桑,等.2014.西藏班公湖蛇绿混杂岩中火山岩锆石U-Pb年代学及地球化学特征[J].大地构造与成矿学,38(1):157~167.
(1)江西省地质调查研究院. 2004. 1∶25万日土县幅地质图.
(2)四川省地质调查院. 2003. 1∶25万革吉县幅地质图.
(1)吴建亮,刘文,尹显科,等.藏北班公湖-怒江缝合带西段沙木罗组火山岩年代学、Hf同位素及地球化学特征.岩石学报(复审中).
Banerjee D M and Bhattacharya P.1994.Petrology and geochemistry of greywackes from the Aravalli Supergroup,Rajasthan,India and the tectonic evolution of a Proterozoic sedimentary basin[J].Precambrian Research,67(1~2):11~35.
Bhat M I and Ghosh S K.2001.Geochemistry of the 2.51 Ga old Rampur group pelites,western Himalayas:Implications for their provenance and weathering[J].Precambrian Research,108(1~2):1~16.
Bhatia M R.1985.Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks:Provenance and tectonic control[J].Sedimentary Geology,45(1):97~113.
Bhatia M R and Crook K A W.1986.Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J].Contributions to Mineralogy and Petrology,92(2):181~193.
Bhatia M R and Taylor S R.1981.Trace-element geochemistry and sedimentary provinces:A study from the Tasman Geosyncline,Australia[J].Chemical Geology,33(1):115~125.
Chang C F,Chen N,Coward M P,et al.1986.Preliminary conclusions of the Royal Society and Academia Sinica 1985 geotraverse of Tibet[J].Nature,323:501~507.
Chen Guorong,Liu Hongfei,Jiang Guangwu,et al.2004.Discovery of the Shamuluo Formation in the central segment of the Bangong Co-Nujiang River suture zone,Tibet[J].Geological Bulletin of China,23(2):193~194(in Chinese with English abstract).
Chi Qinghua and Yan Mingcai.2007.Handbook of Elemental Abundance for Applied Geochemistry[M].Beijing:Geological Publishing House,148(in Chinese with English abstract).
Condie K C.1993.Chemical composition and evolution of the upper continental crust:Contrasting results from surface samples and shales[J].Chemical Geology,104(1~4):1~37.
Cox R and Lowe D R.1995.A conceptual review of regional-scale controls on the composition of clastic sediment and the co-evolution of continental blocks and their sedimentary cover[J].Journal of Sedimentary Research Section A-Sedimentary Petrology and Processes,65(1):1~12.
Cox R,Lowe D R and Cullers R L.1995.The influence of sediment recycling and basement composition on evolution of mudrock chemistry in the southwestern United States[J].Geochimica et Cosmochimica Acta,59(14):2 919~2 940.
Cullers R L.1994.The controls on the major and trace element variation of shales,siltstones,and sandstones of Pennsylvanian-Permian age from uplifted continental blocks in Colorado to platform sediment in Kansas,USA[J].Geochimica et Cosmochimica Acta,58(22):4 955~4 972.
Cullers R L and Podkovyrov V N.2000.Geochemistry of the Mesoproterozoic Lakhanda shales in southeastern Yakutia,Russia:implications for mineralogical and provenance control,and recycling[J].Precambrian Research,104(1):77~93.
Du Dedao,Qu Xiaoming,Wang Genhou,et al.2011.Bidirectional subduction of the middle Tethys oceanic basin in the west segment of Bangonghu-Nujiang Suture,Tibet:Evidence from Zircon U-Pb LA-ICPMS dating and petrogeochemistry of arc granites[J].Acta Petrologica Sinica,27(7):1 993~2 002(in Chinese with English abstract).
Fedo C M,Nesbitt H W and Young G M.1995.Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols,with implications for paleoweathering conditions and provenance[J].Geology,23(10):921~924.
Fedo C M,Young G M,Nesbitt H W,et al.1997.Potassic and sodic metasomatism in the Southern Province of the Canadian Shield:Evidence from the Paleoproterozoic Serpent Formation,Huronian Supergroup,Canada[J].Precambrian Research,84(1~2):17~36.
Feng Lianjun,Chu Xuelei,Zhang Qirui,et al.2003.CIA(chemical index of alteration)and its applications in the Neoproterozoic clastic rocks[J].Earth Science Frontiers(China University of Geosciences,Beijing),10(4):539~544(in Chinese with English abstract).
Haskin M A and Haskin L A.1966.Rare Earths in European Shales:ARedetermination[J].Science,154(3 748):507~509.
Hayashi K,Fujisawa H,Holland H D,et al.1997.Geochemistry of similar to 1.9 Ga sedimentary rocks from northeastern Labrador,Canada[J].Geochimica et Cosmochimica Acta,61(19):4 115~4 137.
Huang Qishuai,Shi Rendeng,Ding Binghua,et al.2012.Re-Os isotopic evidence of MOR-type ophiolite from the Bangong Co for the opening of Bangong-Nujiang Tethys Ocean[J].Acta Petrologica et Mineralogica,31(4):465~478(in Chinese with English abstract).
Ishiga H and Dozen K.1997.Geochemical indications of provenance change as recorded in Miocene shales:opening of the Japan Sea,San'in region,southwest Japan[J].Marine Geology,144(1):211~228.
Kapp P,Murphy M A,Yin A,et al.2003.Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet[J].Tectonics,22(4):253.
Liang Sang,Zhou Tao,Li Dewei,et al.2017.Timing of southward subduction of Meso-tethys in Bangong Lake:Constraints from supra-subduction zone(SSZ)-type gabbro[J].Geotectonica et Metallogenia,41(5):989~1 000(in Chinese with English abstract).
Liu D,Huang Q,Fan S,et al.2014.Subduction of the Bangong-Nujiang Ocean:Constraints from granites in the Bangong Co area,Tibet[J].Geological Journal,49(2):188~206.
Liu W,Xia B,Zhong Y,et al.2014.Age and composition of the Rebang Co and Julu ophiolites,central Tibet:Implications for the evolution of the Bangong Meso-Tethys[J].International Geology Review,56(4):430~447.
Liu Z F,Colin C,Huang W,et al.2007.Climatic and tectonic controls on weathering in south China and Indochina Peninsula:Clay mineralogical and geochemical investigations from the Pearl,Red,and Mekong drainage basins[J].Geochemistry,Geophysics,Geosystems,8(5):Q5005.
Mclennan S M.1993.Weathering and global denudation[J].Journal of Geology,101(2):295~303.
Mc Lennan S M,Hemming S R,Mc Daniel D K,et al.1993.Geochemical approaches to sedimentation,provenance,and tectonics[J].Geological Society of America Special Papers,284:21~40.
Mc Lennan S M,Hemming S R,Taylor S R,et al.1995.Early Proterozoic crustal evolution:Geochemical and Nd-Pb isotopic evidence from metasedimentary rocks,southwestern North America[J].Geochimica et Cosmochimica Acta,59(6):1 153~1 177.
Murray R W,Buchholtz Ten Brink M R,Jones D L,et al.1990.Rare earth elements as indicators of different marine depositional environments in chert and shale[J].Geology,18(3):268~271.
Naqvi S M,Sawkar R H,Rao D,et al.1988.Geology,geochemistry and tectonic setting of Archaean greywackes from Karnataka Nucleus,India[J].Precambrian Research,39(3):193~216.
Nesbitt H W and Young G M.1982.Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J].Nature,299(5885):715~717.
Nesbitt H W and Young G M.1989.Formation and diagenesis of weathering profiles[J].Journal of Geology,97(2):129~147.
Nesbitt H W and Young G M.1984.Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J].Geochimica et Cosmochimica Acta,48(7):1 523~1 534.
Nesbitt H W,Young G M,Mc Lennan S M,et al.1996.Effects of chemical weathering and sorting on the petrogenesis of siliciclastic sediments,with implications for provenance studies[J].Journal of Geology,104(5):525~542.
Pan Guitang,Mo Xuanxue,Hou Zengqian,et al.2006.Spatial-temporal Framework of the Gangdese Orogenic Belt and Its Evolution[J].Acta Petrologica Sinica,22(3):521~533(in Chinese with English abstract).
Passchier S and Krissek L A.2008.Oligocene-Miocene Antarctic continental weathering record and paleoclimatic implications,Cape Roberts drilling project,Ross Seal,Antarctica[J].Palaeogeography,Palaeoclimatology,Palaeoecology,260(1~2):30~40.
Plank T and Langmuir C H.1998.The chemical composition of subducting sediment and its consequences for the crust and mantle[J].Chemical Geology,145(3~4):325~394.
Qiu Ruizhao,Zhou Shu,Deng Jingfu,et al.2004.Dating of gabbro in the Shemalagou ophiolite in the western segment of the Bangong CoNujiang ophiolite belt,Tibet:With a discussion of the age of the Bangong Co-Nujiang ophiolite belt[J].Geology in China,31(3):262~268(in Chinese with English abstract).
Qu Xiaoming,Wang Ruijiang,Xin Hongbo,et al.2009.Geochronology and geochemistry of igneous along the Bangong Lake rocks related to the subduction of the Tethys oceanic plate arc zone,the western Tibetan Plateau[J].Geochimica,38(6):523~535(in Chinese with English abstract).
Qu Xiaoming,Xin Hongbo,Zhao Yuanyi,et al.2010.Opening time of Bangong Lake Middle Tethys Oceanic Basin of the Tibet Plateau:Constraints from petro-geochemistry and zircon U-Pb LAICPMS dating of mafic ophiolites[J].Earth Science Frontiers(China University of Geosciences,Beijing),17(3):53~63(in Chinese with English abstract).
Roser B P and Korsch R J.1986.Determination of tectonic setting of sandstone-mudstone suits using SiO2content and K2O/Na2O ratio[J].Journal of Geology,94(5):635~650.
Savoy L E,Stevenson R K and Mountjoy E W.2000.Provenance of Upper Devonian-Lower Carboniferous miogeoclinal strata,southeastern Canadian Cordillera:Link between tectonics and sedimentation[J].Journal of Sedimentary Research,70(1A):181~193.
Scheffler K,Buehmann D and Schwark L.2006.Analysis of Late Palaeozoic glacial to postglacial sedimentary successions in South Africa by geochemical proxies-Response to climate evolution and sedimentary environment[J].Palaeogeography,Palaeoclimatology,Palaeoecology,240(1~2):184~203.
Shao Lei,Li Xianhua,Wei Gangjian,et al.2001.The slope of the South China Sea material sources of the deposit[J].Science in China(Series D),31(10):828~833(in Chinese with English abstract).
Shi Rendeng.2007.The geochronology of SSZ-type ophiolites:Constraints on the evolution time of the Bangong Lake-Nujiang ocean basin[J].Chinese Science Bulletin,52(2):223~227(in Chinese with English abstract).
Sreenivas B and Srinivasan R.1994.Identification of paleosols in the Precambrian metapelitic assemblages of peninsular India major element geochemical approach[J].Current Science,67(2):89~94.
Taylor S R and Mc Lennan S M.1985.The Continental Crust:Its Composition and Evolution[M].Oxford:Blackwell Scientific Publications,312.
Totten M W,Hanan M A and Weaver B L.2000.Beyond whole-rock geochemistry of shales:The importance of assessing mineralogic controls for revealing tectonic discriminants of multiple sediment sources for the Ouachita Mountain flysch deposits[J].Geological Society of A-merica Bulletin,112(7):1 012~1 022.
Wang W,Aitchison J C,Lo C,et al.2008.Geochemistry and geochronology of the amphibolite blocks in ophiolitic mélanges along BangongNujiang suture,central Tibet[J].Journal of Asian Earth Sciences,33(1~2):122~138.
Wang Xibin.1987.Lithospheric Evolution of Himalayan:Tibet Ophiolites[M].Beijing:Geological Publishing House,336(in Chinese with English abstract).
Wani H and Mondal M E A.2011.Evaluation of provenance,tectonic setting,and paleoredox conditions of the Mesoproterozoic-Neoproterozoic basins of the Bastar craton,Central Indian Shield:Using petrography of sandstones and geochemistry of shales[J].Lithosphere,3(2):143~154.
Xie Bingjing,Cheng Jie and Huang Chuanguan.2010.The found and the significance for the west area of Samut Luo Group in the Bangong Lake-Nu River suture[J].Journal of East China Institute of Technology,33(2):159~164(in Chinese with English abstract).
Xu Wenli,Zheng Rongcai,Yan Xue,et al.2014.Trace and rare earth element geochemistry of the Early Paleozoic black shales in the Lower Yangtze area and its geological significances[J].Journal of Jilin University(Earth Science Edition),44(4):1 108~1 122(in Chinese with English abstract).
Yang S Y,Yim W W S and Huang G Q.2008.Geochemical composition of inner shelf quaternary sediments in the northern South China Sea with implications for provenance discrimination and paleoenvironmental reconstruction[J].Global and Planetary Change,60(3~4):207~221.
Yin A and Harrison T M.2000.Geologic evolution of the Himalayan-Tibetan orogen[J].Annual Review of Earth and Planetary Sciences,28:211~280.
Young G M and Nesbitt H W.1999.Paleoclimatology and provenance of the glaciogenic Gowganda Formation(Paleoproterozoic),Ontario,Canada:A chemostratigraphic approach[J].Geological Society of America Bulletin,111(2):264~274.
Zhang H.1988.The structure of the 1985 Tibet geotraverse,Lhasa to Golmud:Appendix,structures and fabrics in the Kunlun Shan:Evidence for Mid-Palaeozoic(Pre-Upper Devonian)deformation[J].Philosophical Transactions of The Royal Society A Mathematical Physical and Engineering Sciences,327(1 594):334~336.
Zhang Jingliang and Zhang Xin.2006.The Element geochemical features of ancient oceanic sedimentary environments in the Silurian period in the Tarim Basin[J].Periodical of Ocean University of China,36(2):200~208(in Chinese with English abstract).
Zhang K,Xia B,Wang G,et al.2004.Early Cretaceous stratigraphy,depositional environments,sandstone provenance,and tectonic setting of central Tibet,western China[J].Geological Society of America Bulletin,116(9):1 202.
Zhang Yuxiu.2007.Tectonic Evoiution of the Middle-western BangongNujiang Suture,Tibet(PHD Dissertation)[D].Guangzhou:Graduate School of the Chinese Academy of Sciences(in Chinese with English abstract).
Zhao Zhenhua.2016.The Elements of the Trace Element Geochemistry[M].Beijing:Science Press,534(in Chinese with English abstract).
Zhou Tao,Chen Chao,Liang Sang,et al.2014.Zircon U-Pb geochronology and geochemical characteristics of volcanic rocks in the ophiolite melange at the Bangong Lake,Tibet[J].Geotectonica et Metallogenia,38(1):157~167(in Chinese with English abstract).
Zhu D,Zhao Z,Niu Y,et al.2013.The origin and pre-Cenozoic evolution of the Tibetan Plateau[J].Gondwana Research,23(4):1 429~1 454.
陈国荣,刘鸿飞,蒋光武,等.2004.西藏班公湖-怒江结合带中段沙木罗组的发现[J].地质通报,23(2):193~194.
迟清华,鄢明才.2007.应用地球化学元素丰度数据手册[M].北京:地质出版社,148.
杜德道,曲晓明,王根厚,等.2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据[J].岩石学报,27(7):1 993~2 002.
冯连君,储雪蕾,张启锐,等.2003.化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用[J].地学前缘,10(4):539~544.
黄启帅,史仁灯,丁炳华,等.2012.班公湖MOR型蛇绿岩Re-Os同位素特征对班公湖-怒江特提斯洋裂解时间的制约[J].岩石矿物学杂志,31(4):465~478.
梁桑,周涛,李德威,等.2017.班公湖中特提斯洋向南俯冲的时限:来自SSZ型辉长岩的制约[J].大地构造与成矿学,41(5):989~1 000.
潘桂棠,莫宣学,侯增谦,等.2006.冈底斯造山带的时空结构及演化[J].岩石学报,22(3):521~533.
邱瑞照,周肃,邓晋福,等.2004.西藏班公湖-怒江西段舍马拉沟蛇绿岩中辉长岩年龄测定---兼论班公湖-怒江蛇绿岩带形成时代[J].中国地质,31(3):262~268.
曲晓明,王瑞江,辛洪波,等.2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学[J].地球化学,38(6):523~535.
曲晓明,辛洪波,赵元艺,等.2010.西藏班公湖中特提斯洋盆的打开时间:镁铁质蛇绿岩地球化学与锆石U-Pb LA-ICP-MS定年结果[J].地学前缘,17(3):53~63.
邵磊,李献华,韦刚健,等.2001.南海陆坡高速堆积体的物质来源[J].中国科学(D辑:地球科学),31(10):828~833.
史仁灯.2007.班公湖SSZ型蛇绿岩年龄对班-怒洋时限的制约[J].科学通报,52(2):223~227.
王希斌.1987.喜马拉雅岩石圈构造演化---西藏蛇绿岩[J].北京:地质出版社,336.
谢冰晶,程捷,黄传冠.2010.班公湖怒江结合带西段沙木罗组的发现及意义[J].东华理工大学学报(自然科学版),33(2):159~164.
徐文礼,郑荣才,颜雪,等.2014.下扬子地区早古生代黑色岩系地球化学特征及其地质意义[J].吉林大学学报(地球科学版),44(4):1 108~1 122.
张玉修.2007.班公湖-怒江缝合带中西段构造演化[D].广州:广州地球化学研究所.
张金亮,张鑫.2006.塔里木盆地志留系古海洋沉积环境的元素地球化学特征[J].中国海洋大学学报(自然科学版),36(2):200~208.
赵振华.2016.微量元素地球化学原理[M].北京:科学出版社,534.
周涛,陈超,梁桑,等.2014.西藏班公湖蛇绿混杂岩中火山岩锆石U-Pb年代学及地球化学特征[J].大地构造与成矿学,38(1):157~167.
(1)江西省地质调查研究院. 2004. 1∶25万日土县幅地质图.
(2)四川省地质调查院. 2003. 1∶25万革吉县幅地质图.
(1)吴建亮,刘文,尹显科,等.藏北班公湖-怒江缝合带西段沙木罗组火山岩年代学、Hf同位素及地球化学特征.岩石学报(复审中).