Origin of the late Paleoproterozoic low-delta O-18 A-type granites on the southern margin of the North China Craton and their geodynamic mechanism
Deng, Xiaoqin; Peng, Touping; Zhou, Yanyan; Zhao, Taiping; Qiu, Zhili
刊名PRECAMBRIAN RESEARCH
2020
卷号351页码:105960
ISSN号0301-9268
DOI10.1016/j.precamres.2020.105960
WOS研究方向Geology
语种英语
WOS记录号WOS:000595149400015
内容类型期刊论文
源URL[http://ir.gig.ac.cn/handle/344008/57314]  
专题同位素地球化学国家重点实验室
中国科学院矿物学与成矿学重点实验室
推荐引用方式
GB/T 7714
Deng, Xiaoqin,Peng, Touping,Zhou, Yanyan,et al. Origin of the late Paleoproterozoic low-delta O-18 A-type granites on the southern margin of the North China Craton and their geodynamic mechanism[J]. PRECAMBRIAN RESEARCH,2020,351:105960.
APA Deng, Xiaoqin,Peng, Touping,Zhou, Yanyan,Zhao, Taiping,&Qiu, Zhili.(2020).Origin of the late Paleoproterozoic low-delta O-18 A-type granites on the southern margin of the North China Craton and their geodynamic mechanism.PRECAMBRIAN RESEARCH,351,105960.
MLA Deng, Xiaoqin,et al."Origin of the late Paleoproterozoic low-delta O-18 A-type granites on the southern margin of the North China Craton and their geodynamic mechanism".PRECAMBRIAN RESEARCH 351(2020):105960.
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