GIG OpenIR  > 中科院广州地化所(2009-)  > 期刊论文
刘兆; 仝来喜
阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据
Source Publication岩石学报
ISSN1000-0569
2015
Volume31Issue:6Pages:1761-1773
Indexed BySCI
Language中文
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/31783
Collection中科院广州地化所(2009-)_期刊论文
Recommended Citation
GB/T 7714
刘兆,仝来喜. 阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据[J]. 岩石学报,2015,31(6):1761-1773.
APA 刘兆,&仝来喜.(2015).阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据.岩石学报,31(6),1761-1773.
MLA 刘兆,et al."阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据".岩石学报 31.6(2015):1761-1773.
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