GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室
陈谋[1,2]; 王核[1]; 张晓宇[1,2]; 闫庆贺[1,2]; 高昊[1,2]
新疆康西瓦伟晶岩的成矿潜力判断:来自锆石U-Pb年代学、地球化学与Hf同位素证据
Source Publication岩石学报
ISSN1000-0569
2022
Volume38Issue:7Pages:2095-2112
Language中文
WOS IDWOS:000878167100016
Indexed BySCI ; EI ; CSCD
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/68755
Collection中国科学院矿物学与成矿学重点实验室
Affiliation1.中国科学院广州地球化学研究所矿物学与成矿学重点实验室,广州510640
2.中国科学院大学,北京100049
Recommended Citation
GB/T 7714
陈谋[1,2],王核[1],张晓宇[1,2],等. 新疆康西瓦伟晶岩的成矿潜力判断:来自锆石U-Pb年代学、地球化学与Hf同位素证据[J]. 岩石学报,2022,38(7):2095-2112.
APA 陈谋[1,2],王核[1],张晓宇[1,2],闫庆贺[1,2],&高昊[1,2].(2022).新疆康西瓦伟晶岩的成矿潜力判断:来自锆石U-Pb年代学、地球化学与Hf同位素证据.岩石学报,38(7),2095-2112.
MLA 陈谋[1,2],et al."新疆康西瓦伟晶岩的成矿潜力判断:来自锆石U-Pb年代学、地球化学与Hf同位素证据".岩石学报 38.7(2022):2095-2112.
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