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GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室
黄旭栋; 陆建军; Stanislas Sizaret; 王汝成; 马东升; 章荣清; 赵旭; 吴劲薇
南岭中-晚侏罗世含铜铅锌与含钨花岗岩的成因差异: 以湘南铜山岭和魏家矿床为例
Source Publication中国科学. 地球科学
ISSN1674-7240
2017
Volume47Issue:7Pages:766-782
Language中文
CSCD IDCSCD:6045916
Indexed ByCSCD
Citation statistics
Cited Times:8[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/34708
Collection中国科学院矿物学与成矿学重点实验室
Recommended Citation
GB/T 7714		 黄旭栋,陆建军,Stanislas Sizaret,等. 南岭中-晚侏罗世含铜铅锌与含钨花岗岩的成因差异: 以湘南铜山岭和魏家矿床为例[J]. 中国科学. 地球科学,2017,47(7):766-782.
APA 黄旭栋.,陆建军.,Stanislas Sizaret.,王汝成.,马东升.,...&吴劲薇.(2017).南岭中-晚侏罗世含铜铅锌与含钨花岗岩的成因差异: 以湘南铜山岭和魏家矿床为例.中国科学. 地球科学,47(7),766-782.
MLA 黄旭栋,et al."南岭中-晚侏罗世含铜铅锌与含钨花岗岩的成因差异: 以湘南铜山岭和魏家矿床为例".中国科学. 地球科学 47.7(2017):766-782.
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