GIG OpenIR  > 中科院广州地化所(2009-)  > 期刊论文
黄文龙; 刘希军; 时毓; 许继峰; 廖帅; 郭琳; 吴伟男; 李政林; 梁琼丹
桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?
Source Publication地质通报
ISSN1671-2552
2015
Volume34Issue:2-3Pages:474-486
Indexed ByCSCD
Language中文
CSCD IDCSCD:5392146
Citation statistics
Cited Times:5[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/31382
Collection中科院广州地化所(2009-)_期刊论文
Recommended Citation
GB/T 7714
黄文龙,刘希军,时毓,等. 桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?[J]. 地质通报,2015,34(2-3):474-486.
APA 黄文龙.,刘希军.,时毓.,许继峰.,廖帅.,...&梁琼丹.(2015).桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?.地质通报,34(2-3),474-486.
MLA 黄文龙,et al."桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?".地质通报 34.2-3(2015):474-486.
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z15048.pdf(2596KB)期刊论文作者接受稿暂不开放CC BY-NC-SAApplication Full Text
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