海南岛新生代玄武质熔岩源区中再循环物质及其年龄的限定:来自Hf-Sr-Nd-Pb同位素的制约

	梅盛旺 1,2; 任钟元1
	海南岛新生代玄武质熔岩源区中再循环物质及其年龄的限定:来自Hf-Sr-Nd-Pb同位素的制约
Source Publication	大地构造与成矿学
ISSN	1001-1552
	2019
Volume	43 Issue:5 Pages:1036-1051
Language	中文
CSCD ID	CSCD:6603045
Indexed By	CSCD ; EI
Citation statistics	Cited Times:1[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/57826
Collection	同位素地球化学国家重点实验室
Affiliation	1.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,广东广州510640; 2.中国科学院大学,北京100049
Recommended Citation GB/T 7714	梅盛旺,任钟元. 海南岛新生代玄武质熔岩源区中再循环物质及其年龄的限定:来自Hf-Sr-Nd-Pb同位素的制约[J]. 大地构造与成矿学,2019,43(5):1036-1051.
APA	梅盛旺,&任钟元.(2019).海南岛新生代玄武质熔岩源区中再循环物质及其年龄的限定:来自Hf-Sr-Nd-Pb同位素的制约.大地构造与成矿学,43(5),1036-1051.
MLA	梅盛旺,et al."海南岛新生代玄武质熔岩源区中再循环物质及其年龄的限定:来自Hf-Sr-Nd-Pb同位素的制约".大地构造与成矿学 43.5(2019):1036-1051.

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