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云南脉地田心铜矿床地质特征及找矿标志分析
引用本文:王佳音,祁昌炜,刘磊,靳浩,赵林山,周瑾.云南脉地田心铜矿床地质特征及找矿标志分析[J].地质与资源,2016,25(4):336-338.
作者姓名:王佳音  祁昌炜  刘磊  靳浩  赵林山  周瑾
作者单位:1. 青海省地质调查局, 青海 西宁 810001;2. 青海省地震局, 青海 西宁 810001
摘    要:脉地田心铜矿床位于云南省漾濞县,是一个受断裂控制明显的小型铜矿床,矿体分布于白垩系下统景星组下段.矿体呈脉状产于灰白色中厚层状石英砂岩中,含矿岩石类型简单,以褪色蚀变砂岩为主.矿体规模为小型,矿石氧化率为73.61%~92.64%,属高氧化率矿石.初步推测矿床成因为与“滇西红层”中的层间断层构造蚀变带密切相关的沉积-热液改造型铜矿床.

关 键 词:铜矿床  滇西红层  白垩系下统  找矿标志  沉积-热液改造型  云南省  
收稿时间:2015-11-04

GEOLOGICAL FEATURES AND ORE-SEARCHING INDICATORS OF THE MAIDITIANXIN COPPER DEPOSIT IN YUNNAN PROVINCE
WANG Jia-yin,QI Chang-wei,LIU Lei,JIN Hao,ZHAO Lin-shan,ZHOU Jin.GEOLOGICAL FEATURES AND ORE-SEARCHING INDICATORS OF THE MAIDITIANXIN COPPER DEPOSIT IN YUNNAN PROVINCE[J].Geology and Resources,2016,25(4):336-338.
Authors:WANG Jia-yin  QI Chang-wei  LIU Lei  JIN Hao  ZHAO Lin-shan  ZHOU Jin
Institution:1. Qinghai Bureau of Geological Survey, Xining 810001, China;2. Qinghai Earthquake Administration, Xining 810001, China
Abstract:The small sized Maiditianxin copper deposit, located in Yangbi County, Yunnan Province, is mainly controlled by faults. The orebodies occur in the lower member of Jingxing Formation, Lower Cretaceous (K1j1). The ore veins are hosted in the medium-thick layered quartz sandstone, which is simply fading altered sandstone. The orebodies are small, with oxidation rate between 73.61% and 92.64%, belonging to high oxidation ore. By preliminary analysis, the genesis of the deposit is sedimentary-hydrothermal reformed type, closely related to the interbedded structural alteration zone in the "West Yunnan red beds".
Keywords:copper deposit  West Yunnan red beds  Lower Cretaceous  ore-searching indicator  sedimentary-hydrothermal reformed type  Yunnan Province
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