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Comparison of metallogenesis and resource potential on the eastern margin of the Jiangnan Upheaval between south Anhui (Wannan) and northeast Jiangxi (Gandongbei) provinces
引用本文:ZHOU Taof,YUAN Feng,HOU Mingjin,FAN Yu,DU Jianguo,ZHU Guang,YUE Shucang. Comparison of metallogenesis and resource potential on the eastern margin of the Jiangnan Upheaval between south Anhui (Wannan) and northeast Jiangxi (Gandongbei) provinces[J]. 自然科学进展(英文版), 2004, 14(12): 1080-1087. DOI: 10.1080/10020070412331344841
作者姓名:ZHOU Taof  YUAN Feng  HOU Mingjin  FAN Yu  DU Jianguo  ZHU Guang  YUE Shucang
作者单位:School of Resources and Environment Engineering, Hefei University of Technology, Hefei 230009, China,School of Resources and Environment Engineering, Hefei University of Technology, Hefei 230009, China,Academy of Geological Survery of Anhui Province, Hefei 230001, China,School of Resources and Environment Engineering, Hefei University of Technology, Hefei 230009, China,Academy of Geological Survery of Anhui Province, Hefei 230001, China,School of Resources and Environment Engineering, Hefei University of Technology, Hefei 230009, China,School of Resources and Environment Engineering, Hefei University of Technology, Hefei 230009, China
基金项目:国家自然科学基金,the Survey Project of the National Land and Resource Department,the Anhui Provincial Excellent Youth Science and Technology Foundation,国家自然科学基金
摘    要:The southern and northern parts of the eastern margin of the Jiangnan Upheaval, located in the northeast of Jiangxi Province (Gandongbei) and the south of Anhui Province (Wannan) share many similar characteristics of basement composition and structural evolution. However, the two areas have very different metal endowments and ranges of deposit types. The aim of this paper is to compare the metallogenic conditions of the two areas in order to analyze the reasons for these differences and to estimate the preliminary resource potential of the studied areas. It is concluded that difference of the crust-mantle interactions, especially the Yanshanian magmatism in the two areas, is the main reason resulting in difference in the ore-forming processes between Wannan and Gandongbei. The resource potential of Gandongbei is significantly greater than that of Wannan.

关 键 词:metallogenesis   resource potential   Jiangnan Upheaval   Wannan   Gandongbei

Comparison of metallogenesis and resource potential on the eastern margin of the Jiangnan Upheaval between south Anhui (Wannan) and northeast Jiangxi (Gandongbei) provinces
ZHOU Taofa,YUAN Feng,HOU Mingjin,FAN Yu,DU Jianguo,ZHU Guang,Yue Shucang. Comparison of metallogenesis and resource potential on the eastern margin of the Jiangnan Upheaval between south Anhui (Wannan) and northeast Jiangxi (Gandongbei) provinces[J]. Progress in Natural Science, 2004, 14(12): 1080-1087. DOI: 10.1080/10020070412331344841
Authors:ZHOU Taofa  YUAN Feng  HOU Mingjin  FAN Yu  DU Jianguo  ZHU Guang  Yue Shucang
Affiliation:1. School of Resources and Environment Engineering, Hefei University of Technology, Hefei 230009, China
2. Academy of Geological Survery of Anhui Province, Hefei 230001, China
Abstract:The southern and northern parts of the eastern margin of the Jiangnan Upheaval, located in the northeast of Jiangxi Province (Gandongbei) and the south of Anhui Province (Wannan) share many similar characteristics of basement composition and structural evolution. However, the two areas have very different metal endowments and ranges of deposit types. The aim of this paper is to compare the metallogenic conditions of the two areas in order to analyze the reasons for these differences and to estimate the preliminary resource potential of the studied areas. It is concluded that difference of the crust-mantle interactions, especially the Yanshanian magmatism in the two areas, is the main reason resulting in difference in the ore-forming processes between Wannan and Gandongbei. The resource potential of Gandongbei is significantly greater than that of Wannan.
Keywords:metallogenesis  resource potential  Jiangnan Upheaval  Wannan  Gandongbei
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