塔里木盆地盐下地区奥陶系火山碎屑物质特征
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摘要
奥陶纪是古亚洲洋演化的关键时期,也是塔里木盆地周缘板块构造环境转换的重要时期.然而,南天山洋向北俯冲-消减的时间一直存在争议.通过对保存在塔里木盆地盐下地区奥陶系鹰山组和良里塔格组的火山碎屑物质的岩石学和地球化学特征研究,结合岩相古地理演化格局,约束了南天山洋向北俯冲削减的时间.研究表明,鹰山组碳酸盐岩中主要发育基性沉凝灰岩薄夹层,良里塔格组火山碎屑物质主要为基性火山岩屑.鹰山组和良里塔格组火山碎屑物质的Th/Yb-Ta/Yb图解指示它们来源于活动大陆边缘弧环境.U/Th-Th图解显示大部分样品落在典型弧火山岩区,且多数位于混有沉积物来源的弧火山岩与典型弧火山岩重叠区域,表明研究区火山物质源区曾受到与俯冲相关流体或熔体的改造.Ba/Th-(La/Sm)_n图解进一步表明火山碎屑物质源区具有上地壳沉积物质起源的熔体混染,且良里塔格组沉积时期,火山碎屑物质源区受沉积物起源熔体混染的程度更深,改造得更加明显和强烈.上述地球化学特征表明,在早奥陶世鹰山组沉积时期南天山洋已经俯冲消减,且在晚奥陶世良里塔格组沉积时期处于强烈俯冲期.
The petrologic and geochemical signatures of volcaniclastic material preserved within carbonate platform deposits from boreholes in the Yanxia area of northern Tarim Basin indicate the presence of an active continental margin volcanic arc during the Middle and Late Ordovician.The volcaniclastics within the Middle Ordovician Yingshan Formation occur as thin layers of basic tuffites in which the vitric grains have undergone partial replacement by carbonate and clay.The volcaniclastics within the Upper Ordovician Lianglitage Formation are primarily basic volcanic clasts within oolitic and grainstone shoal deposits.Geochemical ratios,especially those of Th/Yb-Ta/Yb,U/Th-Th and Ba/Th-(La/Sm),fall within the fields for typical volcanic arcs on continental margins and with a variable admixture of fluids that had interacted with pre-volcanic terrestrial sediments.The degree of admixture is greatest in the volcaniclastics within the Lianglitage Formation,which suggests that the inferred subduction of the South Tianshan Ocean crust below the present northern margin of the Tarim plate had begun by Middle Ordovician and had intensified during the Late Ordovician.
The petrologic and geochemical signatures of volcaniclastic material preserved within carbonate platform deposits from boreholes in the Yanxia area of northern Tarim Basin indicate the presence of an active continental margin volcanic arc during the Middle and Late Ordovician.The volcaniclastics within the Middle Ordovician Yingshan Formation occur as thin layers of basic tuffites in which the vitric grains have undergone partial replacement by carbonate and clay.The volcaniclastics within the Upper Ordovician Lianglitage Formation are primarily basic volcanic clasts within oolitic and grainstone shoal deposits.Geochemical ratios,especially those of Th/Yb-Ta/Yb,U/Th-Th and Ba/Th-(La/Sm),fall within the fields for typical volcanic arcs on continental margins and with a variable admixture of fluids that had interacted with pre-volcanic terrestrial sediments.The degree of admixture is greatest in the volcaniclastics within the Lianglitage Formation,which suggests that the inferred subduction of the South Tianshan Ocean crust below the present northern margin of the Tarim plate had begun by Middle Ordovician and had intensified during the Late Ordovician.
引文
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Gao,H.H.,He,D.F.,Tong,X.G.,et al.,2018.Tectonic-Depositional Environment and Petroleum Exploration of Yingshan Formation in the Tarim Basin.Earth Science,43(2):551-565(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.509
Hallberg,J.A.,1984.A Geochemical Aid to Igneous Rock Type Identification in Deeply Weathered Terrain.Journal of Geochemical Exploration,20(1):1-8.https://doi.org/10.1016/0375-6742(84)90085-2
Hastie,A.R.,Kerr,A.C.,Pearce,J.A.,et al.,2007.Classification of Altered Volcanic Island Arc Rocks Using Immobile Trace Elements:Development of the Th-Co Discrimination Diagram.Journal of Petrology,48(12):2341-2357.https://doi.org/10.1093/petrology/egm062
He,D.F.,Zhou,X.Y.,Zhang C.J.,et al.,2007.Tectonic Types and Evolution of Ordovician Proto-Type Basins in the Tarim Region.Chinese Science Bulletin,52(S1):126-135(in Chinese).
Hopsona,C.,Wen,J.,Tilton,G.,et al.,1989.Paleozoic Plutonism in East Junggar,Bogdashan,and Eastern Tianshan,NW China.EOS.Transactions of the American Geophysical Union,70:1403-1404.
Hou,M.C.,Wan,L.,Fu,H.,et al.,2006.Study on the Sedimentary Environment of the Upper Ordovician Lianglitage Formation in the South of Tarim River,China.Journal of Chengdu University of Technology(Science&Technology Edition),33(5):509-516(in Chinese with English abstract).
Li,D.S.,Liang,D.G.,Jia,C.Z.1996.Hydrocarbon Accumulations in the Tarim Basin,China.AAPG Bulletin,80(10):1587-1603.https://doi.org/10.1306/64eda0be-1724-11d7-8645000102c1865d
Lin,C.S.,Liu,J.Y.,Eriksson,K.,et al.,2014.Late Ordovician,Deep-Water Gravity-Flow Deposits,Palaeogeography and Tectonic Setting,Tarim Basin,Northwest China.Basin Research,26(2):297-319.https://doi.org/10.1111/bre.12028
Lin,C.S.,Yang,H.J.,Cai,Z.Z.,et al.,2013.Evolution of Depositional Architecture of the Ordovician Carbonate Platform in the Tarim Basin and Its Response to Basin Processes.Acta Sedimentologica Sinica,31(5):907-919(in Chinese with English abstract).
Lou,X.Y.,Xu,X.S.,2004.Tectonic-Sedimentary Responses of the Tarim Basin,Xinjiang during the Late Early Palaeozoic.Sedimentary Geology and Tethyan Geology,24(3):72-79(in Chinese with English abstract).
Pearce,J.A.,1983.The Role of Sub-Continental Lithosphere in Magma Genesis at Destructive Plate Margins.In:Hawkesworth,C.J.,Norry,M.J.,eds.,Continental Basalts and Mantle Xenoliths.Shiva,Nantwich.
Ramsey,M.H.,Potts,P.J.,Webb,P.C.,et al.,1995.An Objective Assessment of Analytical Method Precision:Comparison of ICP-AES and XRF for the Analysis of Silicate Rocks.Chemical Geology,124(1-2):1-19.https://doi.org/10.1016/0009-2541(95)00020-m
Shi,K.B.,Jiang,Q.C.,Liu,B.,et al.,2017.Sedimentary Characteristics and Evolution of Cambrian-Ordovician in Quruqtagh Area,NE Tarim Basin,Xinjiang.Acta Petrologica Sinica,33(4),1204-1220(in Chinese with English abstract).
Sun,S.J.,Zhang,L.P.,Ding,X.,2015.Zircon U-Pb Ages,Hf Isotopes and Geochemical Characteristics of Volcanic Rocks in Nagqu Area,Tibet and Their Petrogenesis.Acta Petrologica Sinica,31(7),2063-2077(in Chinese with English abstract).
Tang,L.J.,1994.Evolution and Tectonic Patterns of Tarim Basin.Earth Science,19(6):742-754(in Chinese with English abstract).
Tang,L.J.,1997a.A Discussion on Paleozoic Tectonic Evolution of Tarim Basin,Northwest China.Geoscience,11(1):15-21(in Chinese with English abstract).
Tang,L.J.,1997b.Major Evolutionary Stages of Tarim Basin in Phanerozoic Time.Earth Science Frontiers,4(3-4):318-324(in Chinese with English abstract).
Tatsumi,Y.,2006.High-Mg Andesites in the Setouchi Volcanic Belt,Southwestern Japan:Analogy to Archean Magmatism and Continental Crust Formation?Annual Review of Earth and Planetary Sciences,34(1):467-499.https://doi.org/10.1146/annurev.earth.34.031405.125014
Wang,S.Y.,Huang,J.W.,Jiang,X.Q.,2006.The Sedimentary and Palaeogeographic Characteristics of the Upper Ordovician in the Tarim Basin.Petroleum Geology&Experiment,28(3):236-242,248(in Chinese with English abstract).
Winchester,J.A.,Floyd,P.A.,1977.Geochemical Discrimination of Different Magma Series and Their Differentiation Products Using Immobile Elements.Chemical Geology,20:325-343.https://doi.org/10.1016/0009-2541(77)90057-2
Xiao,X.C.,Tang,Y.Q.,Li,J.Y.,et al.,1991.Tectonic Evolution of the Southern Margin of the Paleo-Central Asian Composite Giant Suture Belt.Beijing Science and Technology Press,Beijing(in Chinese).
Xu,Z.Q.,He,B.Z.,Zhang,C.L.,et al.,2013.Tectonic Framework and Crustal Evolution of the Precambrian Basement of the Tarim Block in NW China:New Geochronological Evidence from Deep Drilling Samples.Precambrian Research,235:150-162.https://doi.org/10.1016/j.precamres.2013.06.001
Yang,T.N.,Li,J.Y.,Sun,G.H.,et al.,2006.Earlier Devonian Active Continental Arc in Central Tianshan:Evidence of Geochemical Analyses and Zircon SHRIMP Dating on Mylonitized Granitic Rock.Acta Petrologica Sinica,22(1):41-48(in Chinese with English abstract).
Yu,B.S.,Lin,C.S.,Fan,T.L.,et al.,2011.Sedimentary Response to Geodynamic Reversion in Tarim Basin during Cambrian and Ordovician and Its Significance to Reservoir Development.Earth Science Frontiers,18(3):221-232(in Chinese with English abstract).
Yue,Y.,Tian,J.C.,Zhao,Y.Q.,et al.,2018.Control of Hetian Paleo-Uplift on Hydrocarbon Accumulation of Ordovician,Tarim Basin.Earth Science,43(11):4215-4225(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2018.253
Zhang,C.L.,Zou,H.B.,Li,H.K.,et al.,2013.Tectonic Framework and Evolution of the Tarim Block in NWChina.Gondwana Research,23(4):1306-1315.https://doi.org/10.1016/j.gr.2012.05.009
Zhang,G.Y.,Liu,W.,Zhang,L.,et al.,2015.Cambrian-Ordovician Prototypic Basin,Paleogeography and Petroleum of Tarim Craton.Earth Science Frontiers,22(3),269-276(in Chinese with English abstract).
Zhang,L.J.,Li,Y.,Zhou,C.G.,et al.,2007.Lithofacies Paleogeographical Characteristics and Reef-Shoal Distribution during the Ordovician in the Tarim Basin.Oil&Gas Geology,28(6):731-737(in Chinese with English abstract).
Zhao,Z.J.,2015.Indicators of Global Sea-Level Change and Research Methods of Marine Tectonic Sequences:Take Ordovician of Tarim Basin as an Example.Acta Petrolei Sinica,36(3):262-273(in Chinese with English abstract).
Zhao,Z.J.,Wu,X.N.,Pan,W.Q.,et al.,2009.Sequence Lithofacies Paleogeography of Ordovician in Tarim Basin.Acta Sedimentologica Sinica,27(5):939-955(in Chinese with English abstract).
Zhu,Z.X.,Wang,K.Z.,Zheng,Y.J.,et al.,2006.Zircon SHRIMP Dating of Silurian and Devonian Granitic Intrusions in the Southern Yili Block,Xinjiang and Preliminary Discussion on Their Tectonic Setting.Acta Petrologica Sinica,22(5):1193-1200(in Chinese with English abstract).
高华华,何登发,童晓光,等,2018.塔里木盆地鹰山组沉积期构造-沉积环境与原型盆地特征.地球科学,43(2):551-565.https://doi.org/10.3799/dqkx.2017.509
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