GIG OpenIR  > 中科院广州地化所(2009-)  > 期刊论文
陈衍景; 李诺
大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异
Source Publication岩石学报
ISSN1000-0569
2009
Volume25Issue:10Pages:2477-2508
Indexed BySCI
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/14779
Collection中科院广州地化所(2009-)_期刊论文
Recommended Citation
GB/T 7714
陈衍景,李诺. 大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异[J]. 岩石学报,2009,25(10):2477-2508.
APA 陈衍景,&李诺.(2009).大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异.岩石学报,25(10),2477-2508.
MLA 陈衍景,et al."大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异".岩石学报 25.10(2009):2477-2508.
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