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The Electrical Conductivity Structure of the Lanping–Simao Basin and its Implications for Mineralization
引用本文:LI Yike,WANG Anjian,CAO Dianhu,GUAN Ye. The Electrical Conductivity Structure of the Lanping–Simao Basin and its Implications for Mineralization[J]. 《地质学报》英文版, 2016, 90(3): 1055-1056. DOI: 10.1111/1755-6724.12750
作者姓名:LI Yike  WANG Anjian  CAO Dianhu  GUAN Ye
作者单位:1 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;2 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
基金项目:This project is financially by the National Science and Technology Support Project (grant No. 2006BAB01B07) and the National Natural Science Foundation of China (grant No. 41202057).
摘    要:正Objective The Lanping–Simao Basin in western Yunnan,located in the southeastern margin of the Tibetan Plateau,is tectonically in the transition zone between the Gondwana and Eurasia tectonic domains.It is also the frontier zone of northeastern extrusion of the Indochina Plate towards the


The Electrical Conductivity Structure of the Lanping–Simao Basin and its Implications for Mineralization
LI Yike,WANG Anjian,CAO Dianhua and GUAN Ye. The Electrical Conductivity Structure of the Lanping–Simao Basin and its Implications for Mineralization[J]. Acta Geologica Sinica (English Edition), 2016, 90(3): 1055-1056. DOI: 10.1111/1755-6724.12750
Authors:LI Yike  WANG Anjian  CAO Dianhua  GUAN Ye
Affiliation:1. Institute of Mineral Resources, Chinese Academy of Geological Sciences, China;2. Institute of Geology, Chinese Academy of Geological Sciences, China
Abstract:
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