GIG OpenIR  > 同位素地球化学国家重点实验室
陶再礼[1,2]; 尹继元[1]; 袁超[3]; 肖文交[4,5]; 陈文[1]; 陈岳龙[2]; 王雅美[1,2]; 杨帆[1,2]
西昆仑造山带晚奥陶世侵入岩的岩石成因:对原特提斯洋俯冲过程的制约
Source Publication岩石学报
ISSN1000-0569
2022
Volume38Issue:11Pages:3321-3340
Language中文
WOS IDWOS:000905326500005
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/344008/68752
Collection同位素地球化学国家重点实验室
Affiliation1.中国地质科学院地质研究所,自然资源部深地动力学重点实验室,北京100037
2.中国地质大学地球科学与资源学院,北京100083
3.中国科学院广州地球化学研究所,同位素地球化学国家重点实验室,广州510640
4.中国科学院新疆生态与地理研究所新疆矿产资源研究中心,乌鲁木齐830011
5.中国科学院地质与地球物理研究所,岩石圈演化国家重点实验室,北京100029
Recommended Citation
GB/T 7714
陶再礼[1,2],尹继元[1],袁超[3],等. 西昆仑造山带晚奥陶世侵入岩的岩石成因:对原特提斯洋俯冲过程的制约[J]. 岩石学报,2022,38(11):3321-3340.
APA 陶再礼[1,2].,尹继元[1].,袁超[3].,肖文交[4,5].,陈文[1].,...&杨帆[1,2].(2022).西昆仑造山带晚奥陶世侵入岩的岩石成因:对原特提斯洋俯冲过程的制约.岩石学报,38(11),3321-3340.
MLA 陶再礼[1,2],et al."西昆仑造山带晚奥陶世侵入岩的岩石成因:对原特提斯洋俯冲过程的制约".岩石学报 38.11(2022):3321-3340.
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