菲律宾马尼拉新生代火山岩的Sr-Nd-Pb-Ca同位素特征:对南海俯冲过程中深部碳循环的制约

	马东东; 刘芳; 祝红丽; 张兆峰; 邓江洪
	菲律宾马尼拉新生代火山岩的Sr-Nd-Pb-Ca同位素特征:对南海俯冲过程中深部碳循环的制约
Source Publication	地球化学
ISSN	0379-1726
	2018
Volume	47 Issue:06 Pages:1508-1514
Language	中文
CSCD ID	CSCD:6390100
Indexed By	CSCD
Citation statistics	Cited Times:2[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/36416
Collection	同位素地球化学国家重点实验室
Recommended Citation GB/T 7714	马东东,刘芳,祝红丽,等. 菲律宾马尼拉新生代火山岩的Sr-Nd-Pb-Ca同位素特征:对南海俯冲过程中深部碳循环的制约[J]. 地球化学,2018,47(06):1508-1514.
APA	马东东,刘芳,祝红丽,张兆峰,&邓江洪.(2018).菲律宾马尼拉新生代火山岩的Sr-Nd-Pb-Ca同位素特征:对南海俯冲过程中深部碳循环的制约.地球化学,47(06),1508-1514.
MLA	马东东,et al."菲律宾马尼拉新生代火山岩的Sr-Nd-Pb-Ca同位素特征:对南海俯冲过程中深部碳循环的制约".地球化学 47.06(2018):1508-1514.

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