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陕西省华县金堆城钼矿床地质特征及控矿条件浅析
引用本文:李建伟,陈世杰,廖俊红,魏明强. 陕西省华县金堆城钼矿床地质特征及控矿条件浅析[J]. 甘肃冶金, 2013, 35(5): 75-79
作者姓名:李建伟  陈世杰  廖俊红  魏明强
作者单位:1. 西北有色地质勘查局七一一总队,陕西汉中,723000
2. 西北有色地勘局七一二总队,陕西咸阳,712000
摘    要:陕西省华县金堆城钼矿床属典型的斑岩型钼矿床。矿体主要赋存在燕山期金堆城花岗斑岩体和中元古界熊耳群的火山岩中,其次为上元古界高山河组变质石英岩中;近东西向断裂构造与斜交东西构造线的平推剪切断裂所构成一个北西-南东向的"节理裂隙密集带",为矿质的富集提供了有利的空间。成矿受上述的地层岩性、构造、侵入岩因素的联合控制。

关 键 词:斑岩型钼矿  金堆城花岗斑岩  地质特征  控矿条件

Geological Features and Oregenesis in Jinduicheng Molybdenum Deposit
LI Jian-wei , CHENG Shi-jie , LIAO Jun-hong , WEI Ming-qiang. Geological Features and Oregenesis in Jinduicheng Molybdenum Deposit[J]. Gansu Metallurgy, 2013, 35(5): 75-79
Authors:LI Jian-wei    CHENG Shi-jie    LIAO Jun-hong    WEI Ming-qiang
Affiliation:1.711 Team of Northwest Non-ferrous Geological and Exploration Bureau,Hanzhong 723000, China; 2.712 Team of Northwest Non-ferrous Geological and Exploration Bureau, Xianyang 712000, China)
Abstract:Jinduicheng molybdenum deposit in Hua County, Shanxi Province is a typical porphyry molybdenum deposit. Ore bodies mainly occurred in Yanshan period in jinduicheng granite porphyry bodies and middle proterozoic Xionger Group of volcanic rock, followed by upper proterozoic Gaoshanhe group metaquartzite ; Nearly east-west fracture structure with oblique east-west tectonic line horizontal pushing shear fracture formed a northwest - southeast joint fissure concentrated beh, provides the advantageous space of mineral enrichment. Mineralization is jointly controlled by the stratum lithology, structure, intrusive rock.
Keywords:porphyry molybdenum deposit  Jinduicheng granite porphyry  geological features  ore-controlling conditions
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