中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Early Paleozoic and Late Mesozoic crustal reworking of the South China Block: Insights from Early Silurian biotite granodiorites and Late Jurassic biotite granites in the Guangzhou area of the south-east Wuyi-Yunkai orogeny

文献类型:期刊论文

作者Liu, Xiao3; Wang, Qiang3,4,5; Ma, Lin3,4,5; Yang, Jin-Hui2; Ma, Yi-Ming1,3; Huang, Tong-Yu3,5
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2021-10-01
卷号219页码:16
ISSN号1367-9120
DOI10.1016/j.jseaes.2021.104890
WOS研究方向Geology
语种英语
WOS记录号WOS:000691732200001
源URL[http://ir.gig.ac.cn/handle/344008/64223]  
专题同位素地球化学国家重点实验室
深地科学卓越创新中心
通讯作者Wang, Qiang; Ma, Lin
作者单位1.China Univ Geosci, Sch Earth Sci, Wuhan 430074, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
4.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China
5.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Liu, Xiao,Wang, Qiang,Ma, Lin,et al. Early Paleozoic and Late Mesozoic crustal reworking of the South China Block: Insights from Early Silurian biotite granodiorites and Late Jurassic biotite granites in the Guangzhou area of the south-east Wuyi-Yunkai orogeny[J]. JOURNAL OF ASIAN EARTH SCIENCES,2021,219:16.
APA Liu, Xiao,Wang, Qiang,Ma, Lin,Yang, Jin-Hui,Ma, Yi-Ming,&Huang, Tong-Yu.(2021).Early Paleozoic and Late Mesozoic crustal reworking of the South China Block: Insights from Early Silurian biotite granodiorites and Late Jurassic biotite granites in the Guangzhou area of the south-east Wuyi-Yunkai orogeny.JOURNAL OF ASIAN EARTH SCIENCES,219,16.
MLA Liu, Xiao,et al."Early Paleozoic and Late Mesozoic crustal reworking of the South China Block: Insights from Early Silurian biotite granodiorites and Late Jurassic biotite granites in the Guangzhou area of the south-east Wuyi-Yunkai orogeny".JOURNAL OF ASIAN EARTH SCIENCES 219(2021):16.

入库方式: OAI收割

来源:广州地球化学研究所

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