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The metallogenic mechanism of the sandstone-type copper deposits in the Chuxiong Basin, Yunnan Province

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【作者】 陈根文夏斌吴延之涂光炽喻亨祥

【Author】 CHEN Genwen XIA Bin WU YanzhiTU Guangzhi,& YU HengxiangGuangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;Open Lab of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China;Department of Geology, Central-South University of Technology, Changsha 410083, China

【机构】 Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, ChinaOpen Lab of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China,Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China,Department of Geology, Central-South University of Technology, Changsha 410083, China,Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

【摘要】 <正> The sandstone-type Cu deposits in the Chuxiong Basin occur in the Cretaceous Gaofengsi Formation and the Maotoushan Formation and the orebodies are stratoid and lenticular in form, structurally controlled by their stratigraphical position. Ore structures are dominated by impregnated and striped ones. In addition, it has been observed that copper mineralization is controlled by water-discharge and deformation structures. Orebodies are commonly seen on the gently inclined limbs of the anticline, with the involution front. Copper mineralization shows a distinct zonation. S, Pb isotope and REE data suggest that the copper would stem from the country rocks and the sulfur largely from the lower strata. During diagenesis oxidized Cu-bearing brines derived from the upper parts and reduced brines from the lower parts are involved in metallogenetic reactions in the stress neutral plane, which is the key to the formation of copper deposits in the Chuxiong Basin.

【Abstract】 The sandstone-type Cu deposits in the Chuxiong Basin occur in the Cretaceous Gaofengsi Formation and the Maotoushan Formation and the orebodies are stratoid and lenticular in form, structurally controlled by their stratigraphical position. Ore structures are dominated by impregnated and striped ones. In addition, it has been observed that copper mineralization is controlled by water-discharge and deformation structures. Orebodies are commonly seen on the gently inclined limbs of the anticline, with the involution front. Copper mineralization shows a distinct zonation. S, Pb isotope and REE data suggest that the copper would stem from the country rocks and the sulfur largely from the lower strata. During diagenesis oxidized Cu-bearing brines derived from the upper parts and reduced brines from the lower parts are involved in metallogenetic reactions in the stress neutral plane, which is the key to the formation of copper deposits in the Chuxiong Basin.

  • 【文献出处】 Science in China(Series D:Earth Sciences) ,中国科学(D辑:地球科学)(英文版) , 编辑部邮箱 ,2000年S1期
  • 【分类号】P618.41
  • 【被引频次】12
  • 【下载频次】147
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