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- W2352626516 abstract "The ophiolite of early Paleozoic time of Beishan in Gansu, affected by the Aljin NE left-lateral strick-slip fault,is divided into three sections which are Baiyunshan-Xichangjing,Tongchangkou-Niuquanzi and Baiyushan-Hongliuhe section Niuquanzi ophiolite, developed all units of ophiolite and resembling eastern Xichangjing and western Hongliuhe ophiolite belonging to the type of oceanic crust ophiolite,is also the type of oceanic crust ophiolite Its Rb-Sr isotope age is 463±18 Ma(middle Ordovician-early stage of late Ordoviaian),the same as age of Rediolaria in band of Xichangjing ophiolite and that of Hongliuhe ophiolite hasn′t been determined Recovering the tectonic,this three secsions are one ophiolite zone of early Paleozoic And it is a stylolitic zone between Tarim and kazakhstan missif in Early Paleozoic" @default.
- W2352626516 created "2016-06-24" @default.
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- W2352626516 date "2001-01-01" @default.
- W2352626516 modified "2023-09-26" @default.
- W2352626516 title "Rb-Sr isotope age of Niuquanzi ophiolite and its tectonic significance in Beishan district,Gansu" @default.
- W2352626516 hasPublicationYear "2001" @default.
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