燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义

GIG OpenIR > 中科院广州地化所(-2008)

	李伍平; 李献华
	燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义
Source Publication	岩石学报
ISSN	1000-0569
	2004
Volume	20 Issue:3 Pages:501-510
Language	中文
Indexed By	sci
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/12513
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	李伍平,李献华. 燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义[J]. 岩石学报,2004,20(3):501-510.
APA	李伍平,&李献华.(2004).燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义.岩石学报,20(3),501-510.
MLA	李伍平,et al."燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义".岩石学报 20.3(2004):501-510.

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