GIG OpenIR  > 中科院广州地化所(-2008)
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
ISSN1000-0569
2004
Volume20Issue:2Pages:351-360
Indexed Bysci
Language中文
Document Type期刊论文
Identifierhttp://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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