北武夷资溪-光泽岩体锆石U-Pb年代学——对确定华南内陆印支期岩浆活动时空分布与形成环境的意义

	覃晓云; 李武显; 岑涛; 吕璞良; 陶继华
	北武夷资溪-光泽岩体锆石U-Pb年代学——对确定华南内陆印支期岩浆活动时空分布与形成环境的意义
Source Publication	大地构造与成矿学
ISSN	1001-1552
	2017
Volume	41 Issue:4 Pages:753-767
DOI	10.16539/j.ddgzyckx.2017.04.009
Indexed By	EI
Language	中文
EI Accession Number	20173504083748
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/34681
Collection	同位素地球化学国家重点实验室
Recommended Citation GB/T 7714	覃晓云,李武显,岑涛,等. 北武夷资溪-光泽岩体锆石U-Pb年代学——对确定华南内陆印支期岩浆活动时空分布与形成环境的意义[J]. 大地构造与成矿学,2017,41(4):753-767.
APA	覃晓云,李武显,岑涛,吕璞良,&陶继华.(2017).北武夷资溪-光泽岩体锆石U-Pb年代学——对确定华南内陆印支期岩浆活动时空分布与形成环境的意义.大地构造与成矿学,41(4),753-767.
MLA	覃晓云,et al."北武夷资溪-光泽岩体锆石U-Pb年代学——对确定华南内陆印支期岩浆活动时空分布与形成环境的意义".大地构造与成矿学 41.4(2017):753-767.

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