中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geochronologic and geochemical evidence for persistence of south-dipping subduction to late Permian time, Langshan area, Inner Mongolia (China): Significance for termination of accretionary orogenesis in the southern Altaids,

文献类型:期刊论文

作者Lin, L. n., W. Xiao, B. Wan, B. F. Windley, S. Ao, C. Han, J. Feng, J. e. Zhang, and Z. Zhang
刊名American Journal of Science
出版日期2014
卷号314页码:679-703
收录类别SCI
版本出版稿
源URL[http://ir.iggcas.ac.cn/handle/132A11/7943]  
专题地质与地球物理研究所_特提斯研究中心
推荐引用方式
GB/T 7714
Lin, L. n., W. Xiao, B. Wan, B. F. Windley, S. Ao, C. Han, J. Feng, J. e. Zhang, and Z. Zhang. Geochronologic and geochemical evidence for persistence of south-dipping subduction to late Permian time, Langshan area, Inner Mongolia (China): Significance for termination of accretionary orogenesis in the southern Altaids,[J]. American Journal of Science,2014,314:679-703.
APA Lin, L. n., W. Xiao, B. Wan, B. F. Windley, S. Ao, C. Han, J. Feng, J. e. Zhang, and Z. Zhang.(2014).Geochronologic and geochemical evidence for persistence of south-dipping subduction to late Permian time, Langshan area, Inner Mongolia (China): Significance for termination of accretionary orogenesis in the southern Altaids,.American Journal of Science,314,679-703.
MLA Lin, L. n., W. Xiao, B. Wan, B. F. Windley, S. Ao, C. Han, J. Feng, J. e. Zhang, and Z. Zhang."Geochronologic and geochemical evidence for persistence of south-dipping subduction to late Permian time, Langshan area, Inner Mongolia (China): Significance for termination of accretionary orogenesis in the southern Altaids,".American Journal of Science 314(2014):679-703.

入库方式: OAI收割

来源:地质与地球物理研究所

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