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
ISSN1000-0569
2004
Volume20Issue:3Pages:501-510
Indexed Bysci
Language中文
Document Type期刊论文
Identifierhttp://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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