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陕西穆家庄铜矿床地质地球化学特征及找矿标志
引用本文:王向阳 樊忠平 党红军. 陕西穆家庄铜矿床地质地球化学特征及找矿标志[J]. 西北地质, 2007, 40(B07): 65-70
作者姓名:王向阳 樊忠平 党红军
作者单位:[1]中国地质大学资源学院,湖北武汉430074 [2]西北有色地质勘查局713总队,陕西商洛726000
摘    要:穆家庄铜矿床形成于柞水.山阳泥盆纪热水沉积盆地中受同生断裂控制的次级深水盆地中,矿体呈透镜状、似层状沿北西西向构造破碎带产出,是秦岭泥盆系中热水沉积一构造改造型的典型矿床之一。在总结矿区地质特征、地球化学特征的基础上,建立了综合找矿标志,为区内找矿提供了新的勘查思路。

关 键 词:穆家庄铜矿 地球化学特征 热水沉积 找矿标志
文章编号:1009-6248(2007)增刊-0065-06
修稿时间:2007-01-252007-04-25

Geological-Geochemical Characteristics and Prospecting Indication of the Mujiazhuang Copper Deposit, Shaanxi Province
WANG Xiang-yang, FAN Zhong-ping, DANG Hong-jun. Geological-Geochemical Characteristics and Prospecting Indication of the Mujiazhuang Copper Deposit, Shaanxi Province[J]. Northwestern Geology, 2007, 40(B07): 65-70
Authors:WANG Xiang-yang   FAN Zhong-ping   DANG Hong-jun
Affiliation:1. Faculty of Earth resources, China University of Geosciences, Wuhan 430074, China; 2. No. 713 Team, Northwesten Bureau for Nonferrous Geological Exploration, Shangluo 726000, China
Abstract:The Mujiazhuang Cu deposit is located in the secondary hydrothermal deposit basin controlled by the contemporaneous faults in the Devonian Zhashui-Shanyang hydrothermal basin. Orebodies occurring in forms of lens and stratabound-like along the NWW-trending structural zone represent the typical deposit of hydrothermal deposit-tectonic alteration in the Devonian strata of the Qinling Mountains. Based on geology and geochemistry, combined prospecting indications for copper deposit in this region are discussed.
Keywords:Mujiazhuang Cu deposit   Hydrothermal deposit   geochemical characteristics   prospecting indications
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