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The latest Jurassic protoliths of the Sangsang mafic schists in southern Tibet: Implications for the spatial extent of Greater India

机译:南部南部的桑刚迈克斯·麦克风分离的最新侏罗纪奖金:对大印度的空间范围的影响

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摘要

Field observations, petrology, zircon geochronology, whole-rock geochemistry, and Sr-Nd isotopes were used to reveal the lithology, age, and tectonic setting of the protoliths of the Sangsang matk schists in the Yarlung Zangbo Suture Zone (YZSZ), central southern Tibet. The mafic schists occur as exotic blocks within the accretionary complex of the YZSZ. Relic amygdaloidal features indicate the schist protoliths were volcanic rocks. The mineral assemblage mainly comprises riebeckite + magnesioriebeckite + chlorite + sericite + albite + relic clinopyroxene. The youngest group of zircon ages constrains the formation time of the protoliths to 1492 2.2 Ma ( i.e., latest Jurassic). Abundant Paleozoic and older zircons suggest the protolith volcanic rocks were erupted onto a continental terrane. Whole -rock geochemical and Sr-Nd isotopic data indicate the protoliths were of ocean island basalt affinity. The mafic schists mostly have high-Ti, alkaline, basaltic compositions with 43.57-46.93 wt% Si02, 3.27-724 wt% Na70 + K20, and 4.04-4.69 wt' Ti02. The schists are enriched in light rare earth elements relative to heavy rare earth elements, and have (LalYb)N 5.85-3.53 and small positive Ta and negative Zr-Hf anomalies. (87Sr/86Sr)i values vary from 0.7044 to 0.7055, while ( mlNcl/m4Ncl)i ranges from 0.512670 to 0.512727, with 01(1(0 values of +44 to +5.5. The protoliths of the mafic schists were probably formed in a within-plate extension setting associated with mantle plume upwelling and melting of continental lithosphere. This setting was related to the Late Jurassic continental breakup of Argoland off the northern margin of east Gondwana, and thus marked the paleoposition of the northern edge of Greater India before the breakup of India from east Gondwana during Early Cretaceous, The N -S extent of Greater India at that time was -2400 km. This further indicates how the India -Eurasia continental convergence has been accommodated. (C) 2019 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
机译:现场观测,岩石学,锆石地理学,全岩地球化学和SR-ND同位素用于揭示南阳桑缝业区(YZSZ),南部中部南阳仓库分类岩的岩性,年龄和构造环境西藏。 MAFIC SCISS在YZSZ的含量复合体内发生异国情调。遗物asygdaloidal特征表明Schist促果蝇是火山岩。矿物组合物主要包括Riebeckite + MagnesiorieBeckite +亚氯酸+绢云母+ Albite + relic Clinoce。最小的锆石年龄将促果实的形成时间约束为1492 2.2 mA(即最新侏罗纪)。丰富的古生代和较旧的锆石建议促果冻火山岩被爆发到大陆特拉内。整体 - 地球化学和SR-ND同位素数据表明促果原是海岛玄武岩亲和力。 MAFIC SCISS主要具有高TI,碱性,玄武岩组合物,具有43.57-46.93wt%SiO 2,3.27-724wt%Na70 + K20和4.04-4.69wt'TIO 2。分类是相对于重稀土元素的轻质稀土元素,具有(LALYB)N 5.85-3.53和小阳性TA和阴性ZR-HF异常。 (87SR / 86SR)I值从0.7044到0.7055变化,而(MLNCL / M4NCL)I范围为0.512670至0.512727,01(1(0值+44至+5.5。可能形成MAFIC SCIST的促果胶)与地幔羽流升高相关的板内延伸设定和大陆岩石圈的熔化。这种环境与东吉隆纳北边缘的Argoland的后期侏罗纪大陆分手有关,从而标志着更多印度北部边缘的古典定位在白垩纪早期的东巩膜中的印度分手,当时的大型印度的N-S范围为-2400公里。这进一步表明了印度欧洲大陆会聚是如何得到容纳的。(c)2019年2019年的Gondwana研究协会。由elsevier bv发布版权所有。

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  • 作者单位

    Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Key Lab Continental Collis &

    Plateau Uplift Inst Tibetan Plateau Res Beijing 100101 Peoples R China;

    Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Key Lab Continental Collis &

    Plateau Uplift Inst Tibetan Plateau Res Beijing 100101 Peoples R China;

    Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Key Lab Continental Collis &

    Plateau Uplift Inst Tibetan Plateau Res Beijing 100101 Peoples R China;

    Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Key Lab Continental Collis &

    Plateau Uplift Inst Tibetan Plateau Res Beijing 100101 Peoples R China;

    Sun Yat Sen Univ Guangdong Prov Key Lab Mineral Resources &

    Geol P Sch Earth Sci &

    Engn Guangzhou 510275 Peoples R China;

    Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Key Lab Continental Collis &

    Plateau Uplift Inst Tibetan Plateau Res Beijing 100101 Peoples R China;

    China Hua You Grp Co Ltd Daqing Co Daqing 163000 Peoples R China;

    Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Key Lab Continental Collis &

    Plateau Uplift Inst Tibetan Plateau Res Beijing 100101 Peoples R China;

    Chinese Acad Sci CAS Ctr Excellence Tibetan Plateau Earth Sci Key Lab Continental Collis &

    Plateau Uplift Inst Tibetan Plateau Res Beijing 100101 Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

    Greater India; Sangsang mafic schists; East Gondwana; Continental breakup; India-Eurasia collision;

    机译:更大的印度;桑康·迈克斯肖特;东吉隆纳;欧式分手;印度 - 欧亚镇碰撞;

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