GIG OpenIR
李孟江; 王仁民; 张莉
华北克拉通北缘尚义地区新太古代TTG成因分析:洋壳玄武岩不同深度下熔融的产物
Source Publication地质通报
ISSN1671-2552
2012
Volume31Issue:5Pages:686-695
Indexed ByCSCD
Language中文
CSCD IDCSCD:4543194
Citation statistics
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/17858
Collection中国科学院广州地球化学研究所
Recommended Citation
GB/T 7714
李孟江,王仁民,张莉. 华北克拉通北缘尚义地区新太古代TTG成因分析:洋壳玄武岩不同深度下熔融的产物[J]. 地质通报,2012,31(5):686-695.
APA 李孟江,王仁民,&张莉.(2012).华北克拉通北缘尚义地区新太古代TTG成因分析:洋壳玄武岩不同深度下熔融的产物.地质通报,31(5),686-695.
MLA 李孟江,et al."华北克拉通北缘尚义地区新太古代TTG成因分析:洋壳玄武岩不同深度下熔融的产物".地质通报 31.5(2012):686-695.
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