New Zircon U-Pb Ages of Mylonitic Granite in the Baluntai Area of the Central Tianshan Block and their Geological Implications
New Zircon U-Pb Ages of Mylonitic Granite in the Baluntai Area of the Central Tianshan Block and their Geological Implications作者机构:School of Earth Sciences and ResourcesChina University of GeosciencesBeijing100083China Key Laboratory of Deep-Earth Dynamics of Ministry of Natural ResourcesInstitute of GeologyChinese Academy of Geological SciencesBeijing 100037China
出 版 物:《Acta Geologica Sinica(English Edition)》 (地质学报(英文版))
年 卷 期:2019年第93卷第4期
页 面:1149-1151页
核心收录:
学科分类:070902[理学-地球化学] 0709[理学-地质学] 0819[工学-矿业工程] 07[理学] 070901[理学-矿物学、岩石学、矿床学] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 0816[工学-测绘科学与技术]
基 金:financially supported by the China Geological Survey(grants No.DD20190001,DD20190004) the Fund from the Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources and the National Science Foundation of China(grants No.41473053,41573045,41873060 and 41830216)
主 题:Pb Block Implications
摘 要:Objective The central Tianshan block mainly consists of the Precambrian metamorphic basement,Ordovician–Silurian meta-sedimentary rocks and Carboniferous–Permian sedimentary rocks.