GIG OpenIR  > 中科院广州地化所(-2008)
李伍平; 李献华; 路凤香
辽西中侏罗世高Sr低Y型火山岩的成因及其地质意义
Source Publication岩石学报
ISSN1000-0569
2001
Volume17Issue:4Pages:523-532
Language中文
Indexed Bysci
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/11773
Collection中科院广州地化所(-2008)
Recommended Citation
GB/T 7714
李伍平,李献华,路凤香. 辽西中侏罗世高Sr低Y型火山岩的成因及其地质意义[J]. 岩石学报,2001,17(4):523-532.
APA 李伍平,李献华,&路凤香.(2001).辽西中侏罗世高Sr低Y型火山岩的成因及其地质意义.岩石学报,17(4),523-532.
MLA 李伍平,et al."辽西中侏罗世高Sr低Y型火山岩的成因及其地质意义".岩石学报 17.4(2001):523-532.
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