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GIG OpenIR  > 同位素地球化学国家重点实验室
郭小飞; 王岳军; 刘汇川; 张玉芝
哀牢山深变质带内两类晚渐新世花岗岩成因及其构造指示
Source Publication中山大学学报. 自然科学版
ISSN0529-6579
2017
Volume56Issue:6Pages:1-14
Language中文
CSCD IDCSCD:6127279
Indexed ByCSCD
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Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/34543
Collection同位素地球化学国家重点实验室
Recommended Citation
GB/T 7714		 郭小飞,王岳军,刘汇川,等. 哀牢山深变质带内两类晚渐新世花岗岩成因及其构造指示[J]. 中山大学学报. 自然科学版,2017,56(6):1-14.
APA 郭小飞,王岳军,刘汇川,&张玉芝.(2017).哀牢山深变质带内两类晚渐新世花岗岩成因及其构造指示.中山大学学报. 自然科学版,56(6),1-14.
MLA 郭小飞,et al."哀牢山深变质带内两类晚渐新世花岗岩成因及其构造指示".中山大学学报. 自然科学版 56.6(2017):1-14.
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