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作 者:XIAO Weifeng WANG Zongxiu CHEN Zhengle HAN Shuqin YU Xinqi
机构地区:[1]Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China [2]School of Earth Sciences and Resources, China University of Geosciences, Beijing, 100083, China
出 处:《Acta Geologica Sinica(English Edition)》2018年第4期1662-1663,共2页地质学报(英文版)
基 金:sponsored by the China Geological Survey(grants No.1212011120335 and 12120114006201)
摘 要:Objective The Late Paleozoic Southern Tianshan Ocean is usually considered to be the last-closed ocean in the Tianshan Orogeny. However, there is still no consensus if this is indeed the case. Blueschist, eclogite and ophiolite are present in the Atbashi Range, Kyrgyzstan, which are believed to be the relics of the Southern Tianshan Ocean. New data obtained through Ar-Ar isotopic analysis in this research provide reliable chronological restrictions for this problem.Objective The Late Paleozoic Southern Tianshan Ocean is usually considered to be the last-closed ocean in the Tianshan Orogeny. However, there is still no consensus if this is indeed the case. Blueschist, eclogite and ophiolite are present in the Atbashi Range, Kyrgyzstan, which are believed to be the relics of the Southern Tianshan Ocean. New data obtained through Ar-Ar isotopic analysis in this research provide reliable chronological restrictions for this problem.
关 键 词:Kyrgyzstan and their Geological Implications New Ar-Ar Isotopic Ages of the Southern Tianshan Mountains
分 类 号:P597[天文地球—地球化学] P618.130.2[天文地球—地质学]
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