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GIG OpenIR  > 中科院广州地化所(-2008)
张传林; 叶海敏; 王爱国; 郭坤一; 董永观
塔里木西南缘新元古代辉绿岩及玄武岩的地球化学特征：新元古代超大型（Rodinia）裂解的证据
Source Publication岩石学报
ISSN1000-0569
2004
Volume20Issue:3Pages:473-482
Language中文
Indexed Bysci
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/12427
Collection中科院广州地化所(-2008)
Recommended Citation
GB/T 7714		 张传林,叶海敏,王爱国,等. 塔里木西南缘新元古代辉绿岩及玄武岩的地球化学特征：新元古代超大型（Rodinia）裂解的证据[J]. 岩石学报,2004,20(3):473-482.
APA 张传林,叶海敏,王爱国,郭坤一,&董永观.(2004).塔里木西南缘新元古代辉绿岩及玄武岩的地球化学特征：新元古代超大型（Rodinia）裂解的证据.岩石学报,20(3),473-482.
MLA 张传林,et al."塔里木西南缘新元古代辉绿岩及玄武岩的地球化学特征：新元古代超大型（Rodinia）裂解的证据".岩石学报 20.3(2004):473-482.
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