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GIG OpenIR  > 中科院广州地化所(-2008)
蓝江波; 徐义刚; 杨启军; 黄小龙
滇西高黎贡带～40Ma OIB型基性岩浆活动：消减特提斯洋片与印度板块断离的产物？
Source Publication岩石学报
ISSN1000-0569
2007
Volume23Issue:6Pages:1334-1346
Language中文
Indexed Bysci
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/13545
Collection中科院广州地化所(-2008)
Recommended Citation
GB/T 7714		 蓝江波,徐义刚,杨启军,等. 滇西高黎贡带～40Ma OIB型基性岩浆活动：消减特提斯洋片与印度板块断离的产物？[J]. 岩石学报,2007,23(6):1334-1346.
APA 蓝江波,徐义刚,杨启军,&黄小龙.(2007).滇西高黎贡带～40Ma OIB型基性岩浆活动：消减特提斯洋片与印度板块断离的产物？.岩石学报,23(6),1334-1346.
MLA 蓝江波,et al."滇西高黎贡带～40Ma OIB型基性岩浆活动：消减特提斯洋片与印度板块断离的产物？".岩石学报 23.6(2007):1334-1346.
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