ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
广西五圩矿田箭猪坡矿床构造变形及演化
  
关键词:tectonic deformation  tectonic evolution  paleostress field restoration  Jianzhupo deposit
基金项目:国家自然科学基金项目(编号: 42072094; 42162012)
作者单位E-mail
张 元 昆明理工大学, 云南昆明 650093
四川省矿产资源勘查集团, 四川成都 610051 
1441547316@qq.com 
陈爱兵 昆明理工大学, 云南昆明 650093 503614694@qq.com 
张庆松 四川省矿产资源勘查集团, 四川成都 610051  
袁 远 广西二一五地质队有限公司, 广西柳州 545006  
刘伯胜 广西二一五地质队有限公司, 广西柳州 545006  
杨 剑 昆明理工大学, 云南昆明 650093  
黄玉洁 昆明理工大学, 云南昆明 650093  
罗连丽 昆明理工大学, 云南昆明 650093  
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摘要:
Tectonic Deformation and Evolution of the Jianzhupo Deposit in Wuxu Ore Field, Guangxi
      Based the research of the tectonic deformation and evolution period of the Jianzhupo deposit, we discuss the tectonic geometry, kinematics and dynamic characteristics of the mining area, to study the controlling effect of tectonic evolution on mineralization. The Jianzhupo deposit area has developed folds, faults and joints, and is characterized by multi-stage activities. The folds contain upright dipping folds and oblique dipping folds, and the axial direction is NW, NE and NS. The faults and joints can be divided into five groups according to the trend: NE, NW, NNW, NS, and EW, and the order of fault formation is NW, NNW→NE→EW→NS, and the joints are mainly sheared joints. There are four main compressive stresses in the study area: NE–SW, NW–SE, EW and NS(NNW). The tectonic evolution of the study area is comprise of four periods, with D2 and D3 (middle and late Yanshan) being the main metallogenic periods. The lateral direction of NNW to the tensile torsional fault and the intersection with the NW fault have good prospecting prospects.
ZHANG Yuan,CHEN Aibing,ZHANG Qingsong,YUAN Yuan,LIU Bosheng,YANG Jian,HUANG Yujie,LUO Lianli.2025.Tectonic Deformation and Evolution of the Jianzhupo Deposit in Wuxu Ore Field, Guangxi[J].Acta Geoscientica Sinica,46(4):711-725.
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