首页|JUNCTION BETWEEN GANJIANG FAULT AND TANLU FAULT AND ITS SIGNIFICANCE TO MINERALIZATION

JUNCTION BETWEEN GANJIANG FAULT AND TANLU FAULT AND ITS SIGNIFICANCE TO MINERALIZATION

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The concept of fault junction is proposed to describe the relationship between the two faults by the authors. The junction relationship between Ganjiang and Tanlu faults is analyzed in this paper, and this has been elucidated through numerical simulation about the tectonic stress field analysis. Numerical simulation of the tectonic stress field conducted for the major mineralization stage of the Jiujiang-Ruichang junction area reveals that the stress field of the junction structure at the major mineralization stage shows a relatively close relationship with the formation of the ore deposits (occurrences).

junction relationshipnumerical simulationJiujiang-Ruichang junction areastructural stress fieldmineralization

CUI Xuejun、XIA Bin、Zeng Zuoxun、Liu Lilin、CHEN Xiangyun、Yang Weiran

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Guangzhou Institute of Geochemistry,Chinese Academy of Science,Guangzhou,GD510640,China

Faculty of Earth Sciences,China University of Geosciences,Wuhan. HB430074,China

Jiangxi Bureau of Geological Survey,Nanchang,JX330002,China

Key Orientation Project for CAS Knowledge Innovation Programproject funded by Ministry of National Land Resources

KZCXZ-SW- 117B2-25

2005

大地构造与成矿学(英文版)
中国科学院广州地球化学研究所

大地构造与成矿学(英文版)

ISSN：1006-513X
年,卷(期)：2005.29(1)
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