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First Report of Zircon U-Pb Chronology and Hf Isotope Evidence of the Heluositan Group Granulite in West Kunlun, Xinjiang

First Report of Zircon U-Pb Chronology and Hf Isotope Evidence of the Heluositan Group Granulite in West Kunlun, Xinjiang

作     者:GUO Xincheng CHEN Bangxue ZHOU Nengwu GAO Jun ZHENG Yuzhuang 

作者机构:No.11 of Geological Party Xinjiang Bureau of Geology and Mineral Exploration and Development 

出 版 物:《Acta Geologica Sinica(English Edition)》 (地质学报(英文版))

年 卷 期:2018年第92卷第2期

页      面:868-869页

核心收录:

学科分类:0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 

基  金:supported by Xinjiang Uygur Autonomous Region 1:50000 special funds to support the transfer(grant No.1212011140056) 

主  题:Hf MS Pb Xinjiang First Report of Zircon U-Pb Chronology and Hf Isotope Evidence of the Heluositan Group Granulite in West Kunlun 

摘      要:Objective As the uplift belt on the southem margin of the Tarim block, the Tiekelike block consists mainly of a set of Precambrian metamorphic rocks with granulite and gneisses. The Heluositan group-complex is the most ancient rock series in the area, and is a key area for studying the formation and evolution of the Precambrian basement of the Tarim craton. LA-ICP-MS zircon U-Pb dating and Hf isotopic analysis of granulite in this area provide new evidence for revealing the formation and evolution of the Precambrian basement in the Tarim Basin.

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