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JIN Xinbiao, WANG Lei, XIANG Hua, LIU Zhongpeng, DUAN Guiling, LI Ziyun. Petrogenesis of diabase from Jiangshiqiao in Taojiang City, Hu'nan Province:Constrains from geochemistry, geochronology and Sr-Nd-Pb isotopes[J]. Geological Bulletin of China, 2017, 36(5): 750-760.
Citation: JIN Xinbiao, WANG Lei, XIANG Hua, LIU Zhongpeng, DUAN Guiling, LI Ziyun. Petrogenesis of diabase from Jiangshiqiao in Taojiang City, Hu'nan Province:Constrains from geochemistry, geochronology and Sr-Nd-Pb isotopes[J]. Geological Bulletin of China, 2017, 36(5): 750-760.
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Petrogenesis of diabase from Jiangshiqiao in Taojiang City, Hu'nan Province:Constrains from geochemistry, geochronology and Sr-Nd-Pb isotopes

  • 1.

    Wuhan Center of Geological Survey, CGS, Wuhan 430205, Hubei, China

  • 2.

    Research Center of Granitic Diagenesis and Mineralization, CGS, Wuhan 430205, Hubei, China

  • 3.

    Team 413, Bureau of Geology and Mineral Exploration and Deveopment of Hu'nan Province, Changde 415000, China

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Received Date:  18 September 2016
Revised Date:  09 March 2017
Publish Date:  25 May 2017
    Abstract

  • Zircon LA-ICP-MS U-Pb dating for diabase from Jiangshiqiao in Taojiang City of Hu'nan Province yielded an emplace-ment age of 229±2.3Ma (n=8, MSWD=1.8, 2σ).The diabase is characterized by low values of potassium (K2O/Na2O=0.14~0.16), and alkali (K2O+Na2O=2.89%~2.96%), enrichment of large ion lithophile elements and LREE and depletion of high field strength el-ements, low (87Sr/86Sr)i ratios (0.70606~0.70644), low positive ε Nd(t) values (1.55~1.87) and enrichment of radioactive Pb, suggesting a mixed source of the depleted mantle (DM) and the lower crustal.In combination with previous studies, the authors hold that the di-abase was formed through partial melt of the mantle and lower crustal components by the upwelling asthenosphere during the Indo-sinian post-orogenic lithosphere extension in Hu'nan Province.

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  • [1] Wang X L, Zhou J C, Qiu J S, et al. LA-ICP-MS U-Pb zircon geochronology of the Neoproterozoic igneous rocks from northern Guangxi, south China:Implications for tectonic evolution[J]. Precambrian Research, 2006, 145:111-130. doi: 10.1016/j.precamres.2005.11.014

    CrossRef Google Scholar

    [2] Li Z X, Zhang L H, Powell C M. South China in Rodinia:part of the missing link between Australia-East Antarctica and Laurentia?[J]. Geology, 1995, 23:407-410. doi: 10.1130/0091-7613(1995)023<0407:SCIRPO>2.3.CO;2

    CrossRef Google Scholar

    [3] Zhao G C, Cawood P A. Tectonothermal evolution of the Mayuan assemblage in the Cathaysia Block:new evidence for Neoproterozo-ic collision-related assembly of the South China craton[J]. American Journal of Science, 1999, 299:309-339. doi: 10.2475/ajs.299.4.309

    CrossRef Google Scholar

    [4] Wang X L, Zhou J C, Griffin W L, et al. Detrital zircon geochronol-ogy of Precambrian basement sequences in the Jiangnan orogen:Dating the assembly of the Yangtze and Cathaysia blocks[J]. Precambrian Research, 2007, 59:117-131.

    Google Scholar

    [5] Zhao J H, Zhou M F, Yan D P, et al. Reappraisal of the ages of Neoproterozoic strata in South China:No connection with the Grenvillian orogeny[J]. Geology, 2011, 39:299-302. doi: 10.1130/G31701.1

    CrossRef Google Scholar

    [6] 孙涛, 刘昌实, 丁兴. 江西三标岩体成因及其地质意义[C]//2004年全国岩石学与地球动力学研讨会. 2004.

    Google Scholar

    [7] Wang X L, Zhou J C, Qiu J S, et al. LA-ICP-MS U-Pb zircon geochronology of the Neoproterozoic igneous rocks from northern Guangxi, South China:Implications for tectonic evolution[J]. Precambrian Research, 2006, 145:111-130. doi: 10.1016/j.precamres.2005.11.014

    CrossRef Google Scholar

    [8] 任纪舜.论中国南部的大地构造[J].地质学报, 1990, 64(4):3-16.

    Google Scholar

    [9] Faure M, Sun Y, Shu L S, et al. Extensional tectonics within a subduction-type orogen. The case study of the Wugongshan dome (Jiangxi Province, southeastern China)[J]. Tectonophysics, 1996, 263:77-106. doi: 10.1016/S0040-1951(97)81487-4

    CrossRef Google Scholar

    [10] Lin W, Wang Q C, Chen K. Phanerozoic tectonics of south China block:New insights from the polyphase deformation in the Yunkai massif[J]. Tectonics, 2008, 27:1-16.

    Google Scholar

    [11] Shu L S, Faure M, Wang B, et al. Late Palaeozoic-Early Mesozoic geological features of South China:Response to the Indosinian collision events in Southeast Asia[J]. C. R. Geoscience, 2008, 340:151-165. doi: 10.1016/j.crte.2007.10.010

    CrossRef Google Scholar

    [12] 舒良树.华南构造演化的基本特征[J].地质通报, 2012, 31(7):1035-1052.

    Google Scholar

    [13] Wang Y J, Zhang Y, Fan W, et al. Structural signatures and 40Ar/39Ar geochronology of the Indosinian Xuefengshan tectonic belt, South China Block[J]. Journal of Structural Geology, 2005, 27(6):985-998. doi: 10.1016/j.jsg.2005.04.004

    CrossRef Google Scholar

    [14] Wang Y J, Fan W M, Cawood P A, et al. Indosinian high-strain deformation for the Yunkaidashan tectonic belt, South China:Kinematics and 40Ar/39Ar geochronological constraints[J]. Tectonics, 2007, 26:1-21.

    Google Scholar

    [15] Wang Y J, Fan W M, Zhang G W, et al. Phanerozoic tectonics of the South China Block:Key observations and controversies[J]. Gondwana Research, 2013, 23:1273-1305. doi: 10.1016/j.gr.2012.02.019

    CrossRef Google Scholar

    [16] Li Z X, Li X H. Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China:a flat-slab subduction model[J]. Geology, 2007, 35:179-182. doi: 10.1130/G23193A.1

    CrossRef Google Scholar

    [17] Chu Y, Faure M, Lin W, et al. Tectonics of the Middle Triassic intracontinental Xuefengshan Belt, South China:new insights from structural and chronological constraints on the basal de'collement zone[J]. International Journal of Earth Sciences, 2012, 101:2125-2150. doi: 10.1007/s00531-012-0780-5

    CrossRef Google Scholar

    [18] Lepvrier C, Faure M, Nguyen V V, et al.North-directed Triassic nappes in Northeastern Vietnam (East Bac Bo)[J]. Journal of Asian Earth Sciences, 2011, 41:56-68. doi: 10.1016/j.jseaes.2011.01.002

    CrossRef Google Scholar

    [19] 金宠. 雪峰陆内构造系统逆冲推滑体系[D]. 青岛: 中国海洋大学博士学位论文, 2010.

    Google Scholar

    [20] 陈世悦.江南-雪峰地区加里东期和印支期不整合分布规律[J].中国地质, 2011, 38(5):1212-1219.

    Google Scholar

    [21] 华仁民, 陈培荣, 张文兰, 等.华南中、新生代与花岗岩类有关的成矿系统[J].中国科学(D辑), 2003, 33(4):335-343.

    Google Scholar

    [22] 毛景文, 谢桂青, 郭春丽, 等.华南地区中生代主要金属矿床时空分布规律和成矿环境[J].高校地质学报, 2008, 14(4):510-526.

    Google Scholar

    [23] 张怀峰, 陆建军, 王汝成, 等.广西栗木大岐岭隐伏花岗岩的成因及其构造意义:岩石地球化学、锆石U-Pb年代学和Nd-Hf同位素制约[J].中国科学(D辑), 2014, 44(5):901-918.

    Google Scholar

    [24] 梁新权, 周云, 蒋英, 等.二叠纪东吴运动的沉积响应差异:来自扬子和华夏板块吴家坪组或龙潭组碎屑锆石LA-ICP-MS UPb年龄研究[J].岩石学报, 2013, 29(10):3592-3606.

    Google Scholar

    [25] Hu L S, Cawood P A, Du Y S, et al. Detrital records for Upper Permian-Lower Triassic succession in the Shiwandashan Basin, South China and implication for Permo-Triassic (Indosinian) orogeny[J]. Journal of Asian Earth Sciences, 2015, 98:152-166. doi: 10.1016/j.jseaes.2014.11.007

    CrossRef Google Scholar

    [26] 张东亮, 黄德志, 张宏法, 等.湘中盆地基底的时代格架:来自锡矿山碎屑锆石U-Pb年龄的证据[J].岩石学报, 2016, 32(11):3456-3468.

    Google Scholar

    [27] 续海金, 马昌前, 钟玉芳, 等. 湖南桃江、大神山花岗岩的锆石SHRIMP定年: 扬子与华夏拼合的时间下限[C]//2004年全国岩石学与地球动力学研讨会论文摘要集. 2004.

    Google Scholar

    [28] 丁兴, 陈培荣, 陈卫峰, 等.湖南沩山花岗岩中锆石LA-ICPMS U-Pb定年:成岩启示和意义[J].中国科学(D辑), 2005, 35(7):606-616.

    Google Scholar

    [29] 彭冰霞, 王岳军, 范蔚茗, 等.湖南中部和广东西部3个典型花岗质岩体的LA-ICPMS锆石U-Pb定年及其成岩意义[J].地质学报, 2006, (10):1597-1597.

    Google Scholar

    [30] Chen W F, Chen P R, Huang H Y, et al. Chronological and geochemical studies of granite and enclave in Baimashan pluton, Hunan, South China[J]. Science in China (Series), 2007, 50(11):1606-1627. doi: 10.1007/s11430-007-0073-1

    CrossRef Google Scholar

    [31] Wang Y J, Fan W M, Sun M, et al. Geochronological, geochemical and geothermal constraints on petrogenesis of the Indosinian peraluminous granites in the South China Block:a case study in the Hunan Province[J]. Lithos, 2007, 96:475-502. doi: 10.1016/j.lithos.2006.11.010

    CrossRef Google Scholar

    [32] 张龙升, 彭建堂, 张东亮, 等.湘西大神山印支期花岗岩的岩石学和地球化学特征[J].大地构造与成矿学, 2012, 36(1):137-148.

    Google Scholar

    [33] 柏道远, 陈必河, 钟响, 等.湘西南印支期五团岩体锆石SHRIMP U-Pb年龄、地球化学特征及形成背景[J].中国地质, 2014, 41(6):2002-2018.

    Google Scholar

    [34] 郭锋, 范蔚茗.湖南省道县虎子岩片麻岩包体的岩石学特征和年代学研究[J].长春地质学院学报, 1997, (1):25-30.

    Google Scholar

    [35] 赵振华, 包志伟, 张伯友.湘南中生代玄武岩类地球化学特征[J].中国科学(D辑), 1998, 28:7-14.

    Google Scholar

    [36] Dai B Z, Jiang S Y, Jiang Y H, et al. Geochronology, geochemistry and Hf-Sr-Nd isotopic compositions of Huziyan mafic xenoliths, southern Hunan Province, South China:Petrogenesis and implications for lower crust evolution[J]. Lithos, 2008, 102(1):65-87.

    Google Scholar

    [37] 刘勇, 李廷栋, 肖庆辉, 等.湘南宁远地区碱性玄武岩形成时代的新证据:锆石LA-ICP-MS U-Pb定年[J].地质通报, 2010, 29(6):833-841.

    Google Scholar

    [38] 刘勇, 李廷栋, 肖庆辉, 等.湘南宜章地区辉绿岩、花岗斑岩、安山岩的形成时代和成因——锆石U-Pb年龄和Hf同位素组成[J].地质通报, 2012, 31(9):1363-1378.

    Google Scholar

    [39] 杨金豹, 赵志丹, 莫宣学, 等.湖南道县虎子岩碱性玄武岩及其基性捕虏体成因和地质意义[J].岩石学报, 2015, 31(5):1421-1432.

    Google Scholar

    [40] Wang X C, Li X H, Li W X, et al. Ca. 825 Ma komatiitic basalts in South China:First evidence for >1500℃ mantle melts by a Rodinian mantle plume[J].Geology, 2007, 35(12):1103-1106. doi: 10.1130/G23878A.1

    CrossRef Google Scholar

    [41] Liu Y S, Hu Z C, Gao S. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257:34-43. doi: 10.1016/j.chemgeo.2008.08.004

    CrossRef Google Scholar

    [42] Liu Y S, Gao S, Hu Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 2010, 51:537-571. doi: 10.1093/petrology/egp082

    CrossRef Google Scholar

    [43] Liu Y S, Hu Z C, Zong K Q, et al. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LAICPMS[J]. Chinese Science Bulletin, 2010, 55:1535-1546. doi: 10.1007/s11434-010-3052-4

    CrossRef Google Scholar

    [44] Ludwig K R. Isoplot 3:a geochronological toolkit for Microsoft excel[M]. Berkeley:Geochronology Centre Special Publication, 2003, 4:1-74.

    Google Scholar

    [45] Wilson B M. Igneous petrogenesis[M]. Springer, 1989:1-457.

    Google Scholar

    [46] Sun S S, McDoonough W. Chemical and istopic systematics of oceanic basslts:implication for mantal composition and processes[J]. Geological Society Special Bulletin, 1989, 42:313-345.

    Google Scholar

    [47] DePaolo D J, Wasserburg G J. Inferences about magma sources and mantle structure from variations of 143Nd/144Nd[J]. Geophysical Research Letters, 1979, 3(12):743-746

    Google Scholar

    [48] Jacobson S B, Wasserburg G J. Sm-Nd isotopic evolution of chondrites[J]. Earth and Planetary Science Letters, 1980, 50(1):139-155. doi: 10.1016/0012-821X(80)90125-9

    CrossRef Google Scholar

    [49] Rollison H R. 岩石地球化学[M]. 杨学明, 杨晓勇, 陈双喜译. 合肥: 中国科学技术大学出版社, 2000.

    Google Scholar

    [50] Hofmann A W, White W M. Mantle plumes from ancient oceanic crust[J]. Earth & Planetary Science Letters, 1982, 57(2):421-436.

    Google Scholar

    [51] Rudnick R L, Gao S.Composit ion of the continental crust[C]//Rudnick R L.Treatise on geochemistry:The crust.Oxford:Elsevier-Pergamon, 2003:1-64.

    Google Scholar

    [52] 王岳军.湖南印支期过铝质花岗岩的形成:岩浆底侵与地壳加厚热效应的数值模拟[J].中国科学(D辑), 2002, 32(6):491-499.

    Google Scholar

    [53] 王岳军, 范蔚茗, 梁新权, 等.湖南印支期花岗岩SHRIMP锆石U-Pb年龄及其成因启示[J].科学通报, 2005, 50(12):1259-1266.

    Google Scholar

    [54] Lepvrier C, Maluski H, Tich V V, et al. The Early Triassic Indosinian orogeny in Vietnam(Truong Son belt and Kontum massif):Implications for the geodynamic evolution of Indochina[J]. Tectonophysics, 2004. 393:87-118. doi: 10.1016/j.tecto.2004.07.030

    CrossRef Google Scholar

    [55] Cawood P A. Terra Australis Orogen:Rodinia breakup and development of the Pacific and Iapetus margins of Gondwana during the Neoproterozoic and Paleozoic[J]. Earth-Science Reviews, 2005. 69(3/4):249-279.

    Google Scholar

    [56] Carter A, Roques D, Bristow C, et al. Understanding Mesozoic accretion in Southeast Asia:Significance of Triassic thermotectonism (Indosinian orogeny) in Vietnam[J]. Geology, 2001, 29:211-214. doi: 10.1130/0091-7613(2001)029<0211:UMAISA>2.0.CO;2

    CrossRef Google Scholar

    [57] Carter A, Clift P D. Was the Indosinian orogeny a Triassic mountain building or thermotectonic reactivation event?[J]. Comptes Rendus Geosciences, 2008, 340:83-93. doi: 10.1016/j.crte.2007.08.011

    CrossRef Google Scholar

    ① 湖南省地质调查院, 益阳幅(H49 C 004003)1: 250000区域地质调查报告. 2002.

    Google Scholar

    ② 湖南省地质调查院, 湖南省区域地质志. 2013.

    Google Scholar

    ③ 湖南省地质调查院, 株洲幅(G49 C 003004)1: 250000区域地质调查报告. 2005.

    Google Scholar

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