四川理塘地区二叠纪洋岛型岩石组合的识别及其构造意义:来自岩石学、地球化学和年代学证据
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摘要
甘孜-理塘蛇绿混杂岩带是西南"三江"构造带的重要组成部分,曾经历了古特提斯构造体系的演化,形成了完整的"沟-弧-盆体系"。本文是首次在甘孜-理塘蛇绿混杂岩带内发现有达森隆洼岩组洋岛型岩石组合,通过详细的岩石学、地球化学、年代学研究表明,达森隆洼岩组主要由枕状玄武岩、灰岩、硅质岩组成,玄武岩SiO_2含量为44.18%～48.82%,富TiO_2含量为2.71%～3.02%,∑REE=141.03×10~(-6)～164.94×10~(-6),轻稀土元素较重稀土元素富集,相对富集Rb、Th、U,亏损Ba、K、Sr,无明显的Nb和Ta异常,稀土元素配分曲线和微量元素蛛网图与典型洋岛玄武岩曲线相似。古生物化石显示该套洋岛型岩石组合沉积时代为二叠纪,锆石U-Pb同位素测年获得枕状玄武岩形成年龄为中二叠世。通过本次研究表明,甘孜-理塘洋盆至少在早二叠世时期就已发育有成熟洋盆。
The Ganzi-Litang ophiolite melange belt,which is an important part of the ‘Three-River'orogenic belt in southwest of China,had experienced the evolution of paleo-tethys and formed one complete trencharc-basin system.This study firstly reports the discovery of Dasenlongwa petrofabric ocean island rock association occurring in the Ganzi-Litang ophiolite melange belt.Detailed petrology,geochemistry and geochronology study shows that the ocean island rock is composed of pillow basalt,limestone and siliceous,and the basalt has SiO_2 of 44.18% ～ 48.82% and high TiO_2 of 2.71%～3.02%.The rock is characterized by a total REE content of 141.03×10~(-6)～164.94×10~(-6),enrichment of LREE relative to HREE,relative enrichment of Rb,Th and U,and depletion of Ba,K and Sr,no distinct anomalies of Nb and Ta.Its REE patterns and the trace element spider diagram are similar to that of typical OIB.Paleontological fossil shows that the sedimentary time of this oceanic island rock is Permian.The SHRIMP II U-Pb dating of zircon from the pillow basalt yields an age of the middle Permian.This research suggests that the Ganzi-Litang oceanic basin had been mature at least in early Permian.
The Ganzi-Litang ophiolite melange belt,which is an important part of the ‘Three-River'orogenic belt in southwest of China,had experienced the evolution of paleo-tethys and formed one complete trencharc-basin system.This study firstly reports the discovery of Dasenlongwa petrofabric ocean island rock association occurring in the Ganzi-Litang ophiolite melange belt.Detailed petrology,geochemistry and geochronology study shows that the ocean island rock is composed of pillow basalt,limestone and siliceous,and the basalt has SiO_2 of 44.18% ～ 48.82% and high TiO_2 of 2.71%～3.02%.The rock is characterized by a total REE content of 141.03×10~(-6)～164.94×10~(-6),enrichment of LREE relative to HREE,relative enrichment of Rb,Th and U,and depletion of Ba,K and Sr,no distinct anomalies of Nb and Ta.Its REE patterns and the trace element spider diagram are similar to that of typical OIB.Paleontological fossil shows that the sedimentary time of this oceanic island rock is Permian.The SHRIMP II U-Pb dating of zircon from the pillow basalt yields an age of the middle Permian.This research suggests that the Ganzi-Litang oceanic basin had been mature at least in early Permian.
引文
Bienvenu P,Bougault H,Joron J L,Treuil M,Dmitriev L.1990.Morb Alteration:Rare-Earth Element/Non-Rare-Earth Hygromagmaphile Element Fractionation.Chemical Geology,82(1~2):1~14.
Cai X F,Cai H L,Liu D M.2006.Stratigraphic Sequences of mixtite series in oceanic islands of orogenic belts and the significance of study.Marine Geology Letters,22(4):9~11(in Chinese with English abstract).
Furman T,Frey F A,Meyer P S.1992.Petrogenesis of evolved basalts and rhyolites at austurhorn,Southeastern Iceland:The role of fractional crystallization.Journal of Petrology,33(6):1405~1445.
Frey F A,Garcia M O and Roden M F.1994.Geochemical characteristics of Koolau Volcano:Implications of intershield geochemical differences among Hawaiian volcanoes.Geochimica et Cosmochimica Acta,58(5):1441~1462.
Feng Q L,Zhang S T,Ge M C,Yan Chengmin,Yu H,Duan G X,Bao J Y.2002.Radiolarians from Hagong formation in Zhongdian,NW Yunnan,and its tectono-paleogeographic implications.Chinese Journal of Geology,37(1):70~78(in Chinese with English abstract).
Hou L W,Fu D M,Dai B C,Xiao Y.1983.Characteristics of magmatic evolution and the relationship with the tectonic plates and endogenic deposit in eastern Tibet-western Sichuan.In:Geological Collected Works of Qinghai-Tibet Plateau(13).Beijing:Geological Publishing House,69~107(in Chinese with English abstract).
Hou Z Q,Hou L W,Ye Q T,Liu F L,Tang G G.1995.Tectonomagmatic Evolution of Yidun Island Arc and Volcanogenic Massive Sulfide Deposits in Sanjiang Region,S.W.China.Beijing:Seismological Press,1~120(in Chinese with English abstract).
Hou Z Q,Lu J R,Li H Y,Wang D H,Lv Q T.1996.Tectonic Evolution of the Tethys in South western China:Is Controlled by Plume Tectonies.Acta Geologica Sinica,17(1):439~453(in Chinese with English abstract).
Hou Z Q,Zaw K,Pan G T,Mo X Xet al.2007.Sanjiang Tethyan metallogenesis in S.W.China:tectonic setting,metallogenic epochs and deposit types.Ore Geology Reviews,31(1~4):48~87.
Hou K J,Li Y H,Tian Y Y.2009.In situ U-Pb zircon dating using laser ablation-multi ion counting-ICP-MS.Mineral Deposits,28(4):481~492(in Chinese with English abstract).
Kimura G,Sakakibara M,Okamura M.1994.Plumes in central Panthalassa Deductions from accreted oceanic fragments in Japan.Tectonics,13(4):905~916.
Kellogg L H,Hager B H,Hilst R D.1999.Compositional stratification in the deep mantle.Science,283(5409):1881~1884.
Kita I,Yamamoto M,Asakawa Y,Nakagawa M,Taguchi S,Hasegawa H.2001.Contemporaneous ascent of within-plate type and island-arc type magmas in the Beppu-Shimabara graben system,Kyushu Island,Japan.Journal of Volcanology and Geothermal Research,111(1~4):99~109.
Liu B T,Jiang Y M,Qu J C.1982.The plate tectonics meaning of discovery of the ancient oceanic crust in Sichuan Litang-Ganzi.In:The Qinghai-Tibet Plateau Geological Collection,12.Beijing:Geological Publishing House,4:119~128(in Chinese with English abstract).
Li X Z,Liu W J,Wang Y Z,Zhu Q W.1999.Tectonic Evolution of the Tethys and Mineralization in the Sanjiang Region,SWChina.Beijing:Geological Publishing House,1~276(in Chinese with English abstract).
Li J L.2004.Basic characteristics of accretion-type orogens.Geological Bulletin of China,23(9):947~951(in Chinese with English abstract).
Lv X C,Ren C C,Wu R,Cheng M,Qiu H,Qiu Y.2016.Discovery of Bimodal Volcanics in Longzi Area,Southern Xizang:Evidences from SHRIMP U-Pb Zircon Age and Geochemical Analysis.Geological Review,62(4):945~954.(in Chinese with English abstract).
Meschede M.1986.A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Y diagram.Chemical Geology,56(3~4):207~218.
Moller A,O’Brien P J,Kennedy A,Kroner A.2003.Linking growth episodes of zircon and metamorphic textures to zircon chemistry:an example from the ultrahigh-temperature granulites of Rogaland(SW Norway).Geological Society of London Special Publications,220(1):65~81.
Mo X X,Lu F X,Shen Y S,Zhu Q W,Hou Z Q,Yang K H,Deng JF,Liu X P,He C X.1993.Sanjiang Tethyan Volcano and Mineralization.Beijing:Geological Publishing House,1~267(in Chinese with English abstract).
Montelli R,Nolet G,Dahlen F A,Masters G,Engdahl E R,Hung SH.2004.Finite-frequency tomography reveals a variety of plumes in the mantle.Science,303(5656):338~343.
Niu Y L.2010.Some basic concepts and problems on the petrogenesis of intra-plate ocean island basalts.Chinese Science Bulletin,52(2):103~114(in Chinese with English abstract).
Pearce J A,Cann J R.1973.Tectonic setting of basic volcanic rocks determined using trace element analyses.Earth&Planetary Science Letters,19(2):290~300.
Pearce J A,Norry M J.1979.Petrogenetic implications of Ti,Zr,Yand Yb variations in volcanic rocks.Contrib.Mineral.Petrol.,69(1):33~47.
Pearce J A.2008.Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archeanoce-anic crust.Lithos,100(1):14~48.
Rubatto D,Gebauer D.2000.Use of Cathodoluminescence for U-Pb Zircon Dating by Ion Microprobe:Some Examples from the Western Alps//Cathodoluminescence in Geosciences.Springer Berlin Heidelberg,373-400.
Rudnick R L,Gao S.2003a.Composition of the continental crust.Treatise on Geochemistry,3:1~64
Rudnick R L,Gao S.2003b.Composition of the continental crust//Rudnick RL.Treatise on Geochemistry(Volume 3).Oxford:Elsevier-Pergamon,1~64.
Sun S S,Mcdonough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.)Magmatism in the Ocean Basins.Geological Society,London,Special Publications,42(1):313~345.
Safonova I,Maruyama S,Hirata T,Kon Y,Rino S.2010.LA ICPMS U-Pb ages of detrital zircons from Russia largest rivers:Implications for major granitoid events in Eurasia and global episodes of supercontinent formation.Journal of Geodynamics,50(3~4):134~153..
Safonova I Y,Santosh M.2014.Accretionary complexes in the AsiaPacific region:Tracing archives of ocean plate stratigraphy and tracking mantle plumes.Gondwana Research,26(1):126~158.
Santosh M.2010.A synopsis of recent conceptual models on supercontinent tectonics in relation to mantle dynamics,life evolution and surface environment.Journal of Geodynamics,50(3):116~133.
Seltmann R,Soloviev S,Shatov V,Pirajno F,Naumov E,Cherkasov S.2010.Metallogeny of Siberia:tectonic,geologic and metallogenic settings of selected significant deposits*.Journal of the Geological Society of Australia,57(6):655~706.
Winchester J A,Floyd P A.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20(77):325~343.
Weaver B L.1991.Teace element evidence for the origin of oceanisland basalts.Geology,19:123~126.
Xu J F,Castillo P R,Li X H,Yu X Y,Zhang B R.2002.MORB-type rocks from the Paleo-Tethyan Mian-Lueyang northern ophiolite in the Qinling Mountains,central China:implications for the source of the low 206Pb/204Pb and high 143Nd/144Nd mantle component in the Indian Ocean.Earth&Planetary Science Letters,198(3~4):323~337.
Yan Z,Li J L,Yong Y,Xiao W J,Wang Z Q,Xiang YS.2008.Tectonic environment of Ordovician carbonate-cherts in the Shihuigou area,North Qilian orogen.Acta Petrologica Sinica,24(10):2384~2394(in Chinese with English abstract).
Yang W Q,Feng Q L,Liu G C.2010.Radiolarian Fauna and Geochemical Characters of the Cherts from Garz-Litang Tectonic Belt and Its Tectono-Paleogeographic Significance.Acta Geologica Sinica,84(1):78~89(in Chinese with English abstract).
Yang G X,Li Y J,Tong L L,Yang B K,Zhang S L,Shen R,Duan FH.2015.New advance in oceanic island basalts of ophiolitic melange from the West Junggar.Acta Geologica Sinica,89(2):392~405(in Chinese with English abstract).
Yang Y Q,Zhao L,Xu Q Q,Zhang R G,Niu B G.2018.Determination of the Hebukesaier Ophiolitic Mélange in the Northern Part of West Junggar and its Tectonic Implications.Acta Geologica Sinica,92(2):298~312(in Chinese with English abstract).
Zou G F.1995.Advance of the research on the Garze-Litang plate junction.Acta Geologica Sichuan,15(4):257~263(in Chinese with English abstract).
Zhong D L.1998.Paleo-Tethys Orogenic Belt in Western YunnanSichuan.Beijing:Science Press,1~231(in Chinese with English abstract).
Zhang S T,Feng Q L,Wang Y Z.2000a.Devonian deep-water sediments in Garze-Litang tectionic belt,19(3):17~20(in Chinese with English abstract).
Zhang S T,Feng Q L.2000b.The Triassic mélange sedlmentation of Zhongdian area.Yunnan geology,19(1):1~7(in Chinese with English abstract).
Zhu D C,Pan G T,Mo X X,Liao Z L,Jiang X S,Wang L Q,Zhao ZD.2005.Geochemistry and petrogenesis of the Sangxiu Formation basalts in the central segment of Tethyan Himalaya.Geochimica,34(1):7~19(in Chinese with English abstract).
Zhu D C,Mo X X,Wang L Q,Zhao Z D,Liao Z L.2008.Hotspotridge interaction for the evolution of Neo-Tethys:Insights from the Late Jurassic-Early Cretaceous magmatism in southern Tibet.Acta Petrologica Sinica,24(2):225~237(in Chinese with English abstract).
蔡雄飞,蔡海磊,刘德民.2006.造山带洋岛混杂岩系地层序列和研究意义.海洋地质动态,22(4):9~11.
冯庆来,张世涛,葛孟春,严城民,余华,段国玺,包俊跃.2002.滇西北中甸地区哈工组放射虫及其构造古地理意义.地质科学,37(1):70~78.
侯立玮,付德明,戴丙春,肖一.1983.藏东川西地区岩浆活动的主要特征及其与板块构造、内生矿产的关系.见:青藏高原地质文集(13).北京:地质出版社,69~107.
侯增谦,侯立纬,叶庆同,刘福禄,唐国光.1995.三江地区义敦岛弧构造-岩浆演化与火山成因块状硫化物矿床.北京:地震出版社,1~120.
侯增谦,卢记仁,李红阳,王登红,吕庆田.1996.中国西南特提斯构造演化-幔柱构造控制.地球学报,17(4):439~453.
侯可军,李延河,田有荣.2009.LA-MC-ICP-MS锆石微区原位U-Pb定年技术.矿床地质,28(4):481~492.
刘宝田,江耀明,曲景川.1982.四川理塘-甘孜一带古洋壳的发现及其对板块构造的意义.见:青藏高原地质文集.北京:地质出版社,4:119~128.
李继亮.2004.增生型造山带的基本特征.地质通报,23(9):947~951.
李兴振,刘文均,王义昭,朱勤文,杜德勋,沈敢富.1999.西南三江地区特提斯构造演化与成矿(总论).北京:地质出版社,1~276.
吕晓春,任冲,武睿,成明,邱海,邱杨.2016.藏南隆子地区早白垩世双峰式火山岩的发现---来自SHRIMP锆石U-Pb年代学和岩石地球化学的证据.地质论评,62(4):945~954.
莫宣学,路凤香,沈上越,朱勤文,侯增谦,杨开辉,邓晋福,刘祥品,何昌祥.1993.三江特提斯火山作用与成矿.北京:地质出版社,1~267.
牛耀龄.2010.板内洋岛玄武岩(OIB)成因的一些基本概念和存在的问题.科学通报,55(2):103~114.
杨文强,冯庆来,刘桂春.2010.滇西北甘孜-理塘构造带放射虫地层、硅质岩地球化学及其构造古地理意义.地质学报,84(1):78~89.
闫臻,李继亮,雍拥,肖文交,王宗起,向永生.2008.北祁连石灰沟奥陶纪碳酸盐岩-硅质岩形成的构造环境.岩石学报,24(10):2384~2394.
杨高学,李永军,佟丽莉,杨宝凯,张胜龙,沈锐,段丰浩.2015.西准噶尔蛇绿混杂岩中洋岛玄武岩研究新进展.地质学报,89(2):392~405.
杨亚琦,赵磊,徐芹芹,郑荣国,牛宝贵.2018.新疆西准噶尔北部和布克赛尔蛇绿混杂岩的厘定及其洋盆闭合时代限定.地质学报,92(2):298~312.
邹光富.1995.甘孜-理塘板块缝合带研究的新进展.四川地质学报,15(4):257~263.
钟大赉.1998.滇川西部古特提斯造山带.北京:科学出版社,1~231.
张世涛,冯庆来,王义昭.2000a.甘孜-理塘构造带泥盆系的深水沉积.地质科技情报,19(3):17~20.
张世涛,冯庆来.2000b.中甸地区三叠系的沉积混杂作用.云南地质,19(1):1~7.
朱弟成,潘桂棠,莫宣学,廖忠礼,江新胜,王立全,赵志丹.2005.特提斯喜马拉雅带中段桑秀组玄武岩的地球化学和岩石成因.地球化学,34(1):7~19.
朱弟成,莫宣学,王立全,赵志丹,廖忠礼.2008.新特提斯演化的热点与洋脊相互作用:西藏南部晚侏罗世-早白垩世岩浆作用推论.岩石学报,24(2):225~237.
Cai X F,Cai H L,Liu D M.2006.Stratigraphic Sequences of mixtite series in oceanic islands of orogenic belts and the significance of study.Marine Geology Letters,22(4):9~11(in Chinese with English abstract).
Furman T,Frey F A,Meyer P S.1992.Petrogenesis of evolved basalts and rhyolites at austurhorn,Southeastern Iceland:The role of fractional crystallization.Journal of Petrology,33(6):1405~1445.
Frey F A,Garcia M O and Roden M F.1994.Geochemical characteristics of Koolau Volcano:Implications of intershield geochemical differences among Hawaiian volcanoes.Geochimica et Cosmochimica Acta,58(5):1441~1462.
Feng Q L,Zhang S T,Ge M C,Yan Chengmin,Yu H,Duan G X,Bao J Y.2002.Radiolarians from Hagong formation in Zhongdian,NW Yunnan,and its tectono-paleogeographic implications.Chinese Journal of Geology,37(1):70~78(in Chinese with English abstract).
Hou L W,Fu D M,Dai B C,Xiao Y.1983.Characteristics of magmatic evolution and the relationship with the tectonic plates and endogenic deposit in eastern Tibet-western Sichuan.In:Geological Collected Works of Qinghai-Tibet Plateau(13).Beijing:Geological Publishing House,69~107(in Chinese with English abstract).
Hou Z Q,Hou L W,Ye Q T,Liu F L,Tang G G.1995.Tectonomagmatic Evolution of Yidun Island Arc and Volcanogenic Massive Sulfide Deposits in Sanjiang Region,S.W.China.Beijing:Seismological Press,1~120(in Chinese with English abstract).
Hou Z Q,Lu J R,Li H Y,Wang D H,Lv Q T.1996.Tectonic Evolution of the Tethys in South western China:Is Controlled by Plume Tectonies.Acta Geologica Sinica,17(1):439~453(in Chinese with English abstract).
Hou Z Q,Zaw K,Pan G T,Mo X Xet al.2007.Sanjiang Tethyan metallogenesis in S.W.China:tectonic setting,metallogenic epochs and deposit types.Ore Geology Reviews,31(1~4):48~87.
Hou K J,Li Y H,Tian Y Y.2009.In situ U-Pb zircon dating using laser ablation-multi ion counting-ICP-MS.Mineral Deposits,28(4):481~492(in Chinese with English abstract).
Kimura G,Sakakibara M,Okamura M.1994.Plumes in central Panthalassa Deductions from accreted oceanic fragments in Japan.Tectonics,13(4):905~916.
Kellogg L H,Hager B H,Hilst R D.1999.Compositional stratification in the deep mantle.Science,283(5409):1881~1884.
Kita I,Yamamoto M,Asakawa Y,Nakagawa M,Taguchi S,Hasegawa H.2001.Contemporaneous ascent of within-plate type and island-arc type magmas in the Beppu-Shimabara graben system,Kyushu Island,Japan.Journal of Volcanology and Geothermal Research,111(1~4):99~109.
Liu B T,Jiang Y M,Qu J C.1982.The plate tectonics meaning of discovery of the ancient oceanic crust in Sichuan Litang-Ganzi.In:The Qinghai-Tibet Plateau Geological Collection,12.Beijing:Geological Publishing House,4:119~128(in Chinese with English abstract).
Li X Z,Liu W J,Wang Y Z,Zhu Q W.1999.Tectonic Evolution of the Tethys and Mineralization in the Sanjiang Region,SWChina.Beijing:Geological Publishing House,1~276(in Chinese with English abstract).
Li J L.2004.Basic characteristics of accretion-type orogens.Geological Bulletin of China,23(9):947~951(in Chinese with English abstract).
Lv X C,Ren C C,Wu R,Cheng M,Qiu H,Qiu Y.2016.Discovery of Bimodal Volcanics in Longzi Area,Southern Xizang:Evidences from SHRIMP U-Pb Zircon Age and Geochemical Analysis.Geological Review,62(4):945~954.(in Chinese with English abstract).
Meschede M.1986.A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Y diagram.Chemical Geology,56(3~4):207~218.
Moller A,O’Brien P J,Kennedy A,Kroner A.2003.Linking growth episodes of zircon and metamorphic textures to zircon chemistry:an example from the ultrahigh-temperature granulites of Rogaland(SW Norway).Geological Society of London Special Publications,220(1):65~81.
Mo X X,Lu F X,Shen Y S,Zhu Q W,Hou Z Q,Yang K H,Deng JF,Liu X P,He C X.1993.Sanjiang Tethyan Volcano and Mineralization.Beijing:Geological Publishing House,1~267(in Chinese with English abstract).
Montelli R,Nolet G,Dahlen F A,Masters G,Engdahl E R,Hung SH.2004.Finite-frequency tomography reveals a variety of plumes in the mantle.Science,303(5656):338~343.
Niu Y L.2010.Some basic concepts and problems on the petrogenesis of intra-plate ocean island basalts.Chinese Science Bulletin,52(2):103~114(in Chinese with English abstract).
Pearce J A,Cann J R.1973.Tectonic setting of basic volcanic rocks determined using trace element analyses.Earth&Planetary Science Letters,19(2):290~300.
Pearce J A,Norry M J.1979.Petrogenetic implications of Ti,Zr,Yand Yb variations in volcanic rocks.Contrib.Mineral.Petrol.,69(1):33~47.
Pearce J A.2008.Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archeanoce-anic crust.Lithos,100(1):14~48.
Rubatto D,Gebauer D.2000.Use of Cathodoluminescence for U-Pb Zircon Dating by Ion Microprobe:Some Examples from the Western Alps//Cathodoluminescence in Geosciences.Springer Berlin Heidelberg,373-400.
Rudnick R L,Gao S.2003a.Composition of the continental crust.Treatise on Geochemistry,3:1~64
Rudnick R L,Gao S.2003b.Composition of the continental crust//Rudnick RL.Treatise on Geochemistry(Volume 3).Oxford:Elsevier-Pergamon,1~64.
Sun S S,Mcdonough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.)Magmatism in the Ocean Basins.Geological Society,London,Special Publications,42(1):313~345.
Safonova I,Maruyama S,Hirata T,Kon Y,Rino S.2010.LA ICPMS U-Pb ages of detrital zircons from Russia largest rivers:Implications for major granitoid events in Eurasia and global episodes of supercontinent formation.Journal of Geodynamics,50(3~4):134~153..
Safonova I Y,Santosh M.2014.Accretionary complexes in the AsiaPacific region:Tracing archives of ocean plate stratigraphy and tracking mantle plumes.Gondwana Research,26(1):126~158.
Santosh M.2010.A synopsis of recent conceptual models on supercontinent tectonics in relation to mantle dynamics,life evolution and surface environment.Journal of Geodynamics,50(3):116~133.
Seltmann R,Soloviev S,Shatov V,Pirajno F,Naumov E,Cherkasov S.2010.Metallogeny of Siberia:tectonic,geologic and metallogenic settings of selected significant deposits*.Journal of the Geological Society of Australia,57(6):655~706.
Winchester J A,Floyd P A.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20(77):325~343.
Weaver B L.1991.Teace element evidence for the origin of oceanisland basalts.Geology,19:123~126.
Xu J F,Castillo P R,Li X H,Yu X Y,Zhang B R.2002.MORB-type rocks from the Paleo-Tethyan Mian-Lueyang northern ophiolite in the Qinling Mountains,central China:implications for the source of the low 206Pb/204Pb and high 143Nd/144Nd mantle component in the Indian Ocean.Earth&Planetary Science Letters,198(3~4):323~337.
Yan Z,Li J L,Yong Y,Xiao W J,Wang Z Q,Xiang YS.2008.Tectonic environment of Ordovician carbonate-cherts in the Shihuigou area,North Qilian orogen.Acta Petrologica Sinica,24(10):2384~2394(in Chinese with English abstract).
Yang W Q,Feng Q L,Liu G C.2010.Radiolarian Fauna and Geochemical Characters of the Cherts from Garz-Litang Tectonic Belt and Its Tectono-Paleogeographic Significance.Acta Geologica Sinica,84(1):78~89(in Chinese with English abstract).
Yang G X,Li Y J,Tong L L,Yang B K,Zhang S L,Shen R,Duan FH.2015.New advance in oceanic island basalts of ophiolitic melange from the West Junggar.Acta Geologica Sinica,89(2):392~405(in Chinese with English abstract).
Yang Y Q,Zhao L,Xu Q Q,Zhang R G,Niu B G.2018.Determination of the Hebukesaier Ophiolitic Mélange in the Northern Part of West Junggar and its Tectonic Implications.Acta Geologica Sinica,92(2):298~312(in Chinese with English abstract).
Zou G F.1995.Advance of the research on the Garze-Litang plate junction.Acta Geologica Sichuan,15(4):257~263(in Chinese with English abstract).
Zhong D L.1998.Paleo-Tethys Orogenic Belt in Western YunnanSichuan.Beijing:Science Press,1~231(in Chinese with English abstract).
Zhang S T,Feng Q L,Wang Y Z.2000a.Devonian deep-water sediments in Garze-Litang tectionic belt,19(3):17~20(in Chinese with English abstract).
Zhang S T,Feng Q L.2000b.The Triassic mélange sedlmentation of Zhongdian area.Yunnan geology,19(1):1~7(in Chinese with English abstract).
Zhu D C,Pan G T,Mo X X,Liao Z L,Jiang X S,Wang L Q,Zhao ZD.2005.Geochemistry and petrogenesis of the Sangxiu Formation basalts in the central segment of Tethyan Himalaya.Geochimica,34(1):7~19(in Chinese with English abstract).
Zhu D C,Mo X X,Wang L Q,Zhao Z D,Liao Z L.2008.Hotspotridge interaction for the evolution of Neo-Tethys:Insights from the Late Jurassic-Early Cretaceous magmatism in southern Tibet.Acta Petrologica Sinica,24(2):225~237(in Chinese with English abstract).
蔡雄飞,蔡海磊,刘德民.2006.造山带洋岛混杂岩系地层序列和研究意义.海洋地质动态,22(4):9~11.
冯庆来,张世涛,葛孟春,严城民,余华,段国玺,包俊跃.2002.滇西北中甸地区哈工组放射虫及其构造古地理意义.地质科学,37(1):70~78.
侯立玮,付德明,戴丙春,肖一.1983.藏东川西地区岩浆活动的主要特征及其与板块构造、内生矿产的关系.见:青藏高原地质文集(13).北京:地质出版社,69~107.
侯增谦,侯立纬,叶庆同,刘福禄,唐国光.1995.三江地区义敦岛弧构造-岩浆演化与火山成因块状硫化物矿床.北京:地震出版社,1~120.
侯增谦,卢记仁,李红阳,王登红,吕庆田.1996.中国西南特提斯构造演化-幔柱构造控制.地球学报,17(4):439~453.
侯可军,李延河,田有荣.2009.LA-MC-ICP-MS锆石微区原位U-Pb定年技术.矿床地质,28(4):481~492.
刘宝田,江耀明,曲景川.1982.四川理塘-甘孜一带古洋壳的发现及其对板块构造的意义.见:青藏高原地质文集.北京:地质出版社,4:119~128.
李继亮.2004.增生型造山带的基本特征.地质通报,23(9):947~951.
李兴振,刘文均,王义昭,朱勤文,杜德勋,沈敢富.1999.西南三江地区特提斯构造演化与成矿(总论).北京:地质出版社,1~276.
吕晓春,任冲,武睿,成明,邱海,邱杨.2016.藏南隆子地区早白垩世双峰式火山岩的发现---来自SHRIMP锆石U-Pb年代学和岩石地球化学的证据.地质论评,62(4):945~954.
莫宣学,路凤香,沈上越,朱勤文,侯增谦,杨开辉,邓晋福,刘祥品,何昌祥.1993.三江特提斯火山作用与成矿.北京:地质出版社,1~267.
牛耀龄.2010.板内洋岛玄武岩(OIB)成因的一些基本概念和存在的问题.科学通报,55(2):103~114.
杨文强,冯庆来,刘桂春.2010.滇西北甘孜-理塘构造带放射虫地层、硅质岩地球化学及其构造古地理意义.地质学报,84(1):78~89.
闫臻,李继亮,雍拥,肖文交,王宗起,向永生.2008.北祁连石灰沟奥陶纪碳酸盐岩-硅质岩形成的构造环境.岩石学报,24(10):2384~2394.
杨高学,李永军,佟丽莉,杨宝凯,张胜龙,沈锐,段丰浩.2015.西准噶尔蛇绿混杂岩中洋岛玄武岩研究新进展.地质学报,89(2):392~405.
杨亚琦,赵磊,徐芹芹,郑荣国,牛宝贵.2018.新疆西准噶尔北部和布克赛尔蛇绿混杂岩的厘定及其洋盆闭合时代限定.地质学报,92(2):298~312.
邹光富.1995.甘孜-理塘板块缝合带研究的新进展.四川地质学报,15(4):257~263.
钟大赉.1998.滇川西部古特提斯造山带.北京:科学出版社,1~231.
张世涛,冯庆来,王义昭.2000a.甘孜-理塘构造带泥盆系的深水沉积.地质科技情报,19(3):17~20.
张世涛,冯庆来.2000b.中甸地区三叠系的沉积混杂作用.云南地质,19(1):1~7.
朱弟成,潘桂棠,莫宣学,廖忠礼,江新胜,王立全,赵志丹.2005.特提斯喜马拉雅带中段桑秀组玄武岩的地球化学和岩石成因.地球化学,34(1):7~19.
朱弟成,莫宣学,王立全,赵志丹,廖忠礼.2008.新特提斯演化的热点与洋脊相互作用:西藏南部晚侏罗世-早白垩世岩浆作用推论.岩石学报,24(2):225~237.