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Forming age and tectono-petrogenises of the Jiugequan ophiolite in the North Qilian Mountain,NW China 被引量:34
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作者 XIA XiaoHong SONG ShuGuang 《Chinese Science Bulletin》 SCIE EI CAS 2010年第18期1899-1907,共9页
The Jiugequan ophiolite is one of the representative ophiolite fragments in the Early Paleozoic orogenic belt of the North Qilian Mountain.It has been drawn much attention and extensively studied in recent years.In th... The Jiugequan ophiolite is one of the representative ophiolite fragments in the Early Paleozoic orogenic belt of the North Qilian Mountain.It has been drawn much attention and extensively studied in recent years.In this study,ion microprobe(SHRIMP) U-Pb dating was carried out for zircons from isotropic gabbro from the Jiugequan ophiolite.Eighteen analyses yield a relatively consistent apparent 206Pb/238U ages from 480 to 508 Ma with a weighted mean age of 490±5 Ma(MSWD=1.06),which is believed to be the crystallization age of the gabbro and thus the forming age of the Jiugequan ophiolite.Major and trace element geochemical study indicates that the diabase-basalts from the Jiugequan ophiolite have N-MORB and E-MORB characteristics with some subduction-related signatures.The petrological,geochemical and chronological data enable us to conclude that the Jiugequan ophiolite is most likely to be formed at a spreading center of back-arc basin during the early Ordovician,while the ancient Qilian oceanic plate subducted northwards.The acquisition of forming age and determination of tectonic setting for Jiugequan ophiolite provide significant constraints on the evolution of intra-oceanic subduction system in the North Qilian orogenic belt during the Early Paleozoic era. 展开更多
关键词 北祁连山 形成时代 蛇绿岩 构造 北祁连造山带 中国 净重 板块俯冲
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北祁连九个泉蛇绿岩及其上覆岩系的岩石地球化学特征和地球动力学意义 被引量:7
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作者 钱青 孙晓猛 +2 位作者 张旗 韩松 贾秀琴 《地质论评》 CAS CSCD 北大核心 1999年第S1期1038-1046,共9页
本文通过对北祁连九个泉蛇绿岩及其上覆岩系的详细的野外、岩石学和地球化学的研究表明:该区火山岩由多个火山角砾岩—块状玄武岩—凝灰岩的旋回所组成;蛇绿岩之上整合覆盖着一套火山岩—沉积岩组合(蛇绿岩的上覆岩系)。蛇绿岩中玄武岩... 本文通过对北祁连九个泉蛇绿岩及其上覆岩系的详细的野外、岩石学和地球化学的研究表明:该区火山岩由多个火山角砾岩—块状玄武岩—凝灰岩的旋回所组成;蛇绿岩之上整合覆盖着一套火山岩—沉积岩组合(蛇绿岩的上覆岩系)。蛇绿岩中玄武岩为典型的N-MORB,其上覆岩系中玄武岩为E-MORB。剖面从下到上,玄武岩中LREE,HFSE含量递增。火山岩的地球化学和沉积岩的岩相学反映了洋壳从扩张中脊向大陆方向迁移的动力学过程,蛇绿岩从形成到侵位的时间间隔较短。 展开更多
关键词 北祁连 九个泉 蛇绿岩 蛇绿岩上覆岩系 岩石地球化学 地球动力学
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