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GIG OpenIR  > 同位素地球化学国家重点实验室
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
ISSN1001-1552
2017
Volume41Issue:4Pages:753-767
DOI10.16539/j.ddgzyckx.2017.04.009
Language中文
EI Accession Number20173504083748
Indexed ByEI
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Document Type期刊论文
Identifierhttp://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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