Geochemistry and geological significance of the 1.8 Ga mafic dyke swarms in the North China Craton: an example from the juncture of Shanxi, Hebei and Inner Mongolia;华北克拉通 1.8Ga 镇铁质岩墙群的地球化学特征 及其地质意义：以晋冀蒙交界地区为例

Yanshi Xuebao/Acta Petrologica Sinica

Volumn 20, Issue 3, 2004, Pages 439-456

  Peng, Peng ^a   Zhai, Ming Guo ^a   Zhang, Hua Feng ^a   Zhao, Tai Ping ^b   Ni, Zhi Yao ^c  

^a BEIJING INSTITUTE OF GEOLOGY FOR MINERAL RESOURCES   (China)

^b GUANGZHOU INSTITUTE OF GEOCHEMISTRY   (China)

^c CHENGDU UNIVERSITY OF TECHNOLOGY   (China)

Author keywords

1.8 Ga; Geochemistry; Mafic dyke swarms; North China Craton; Petrology

Indexed keywords

EID: 85168632956     PISSN: 10000569     EISSN: 20958927     Source Type: Journal    
DOI: 10.0000/e652fe88f6354ef98bd4e58aa0d0e179     Document Type: Article

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