Knowledge Management System Of Guangzhou Institute of Geochemistry,CAS
王强; 赵振华; 许继峰; 白正华; 王建新; 刘成新 | |
鄂东南铜山口、殷祖埃达克质(adakitic)侵入岩的地球化学特征对比:(拆沉)下地壳熔融与斑岩铜矿的成因 | |
Source Publication | 岩石学报 |
ISSN | 1000-0569 |
2004 | |
Volume | 20Issue:2Pages:351-360 |
Language | 中文 |
Indexed By | sci |
Document Type | 期刊论文 |
Identifier | http://ir.gig.ac.cn/handle/344008/12403 |
Collection | 中科院广州地化所(-2008) |
Recommended Citation GB/T 7714 | 王强,赵振华,许继峰,等. 鄂东南铜山口、殷祖埃达克质(adakitic)侵入岩的地球化学特征对比:(拆沉)下地壳熔融与斑岩铜矿的成因[J]. 岩石学报,2004,20(2):351-360. |
APA | 王强,赵振华,许继峰,白正华,王建新,&刘成新.(2004).鄂东南铜山口、殷祖埃达克质(adakitic)侵入岩的地球化学特征对比:(拆沉)下地壳熔融与斑岩铜矿的成因.岩石学报,20(2),351-360. |
MLA | 王强,et al."鄂东南铜山口、殷祖埃达克质(adakitic)侵入岩的地球化学特征对比:(拆沉)下地壳熔融与斑岩铜矿的成因".岩石学报 20.2(2004):351-360. |
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