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吉林省龙井市金谷山金矿床地质特征及成因探讨
引用本文:李德洪,于政涛,扈英彬,牛继辉.吉林省龙井市金谷山金矿床地质特征及成因探讨[J].吉林地质,2005,24(3):11-15.
作者姓名:李德洪  于政涛  扈英彬  牛继辉
作者单位:1. 吉林省地质调查院,吉林,长春,130061
2. 吉林省地质科学研究所,吉林,长春,130012
摘    要:金谷山金矿床产于上古生界二叠系柯岛组地层中,矿化类型为构造蚀变岩型。火山喷发-沉积作用形成的中酸性火山-碎屑岩系,是金矿形成的基本因素和矿源层,变质变形作用是金矿形成的根本因素,脉岩活动是金矿成矿的叠加因素。矿体受韧性剪切变形变质带控制,矿床成因为变质热液与岩浆热液叠加的复合型。

关 键 词:金矿床  地质特征  成因探讨  吉林龙井
文章编号:1001-2427(2005)03-011-05
收稿时间:2005-03-04
修稿时间:2005-03-042005-08-20

Geologic features and genesis of the Jingushan Au deposit, Longjing City, Jilin Province
LI De-hong,YU Zheng-tao,HU Ying-bin,NIU Ji-hui.Geologic features and genesis of the Jingushan Au deposit, Longjing City, Jilin Province[J].Jilin Geology,2005,24(3):11-15.
Authors:LI De-hong  YU Zheng-tao  HU Ying-bin  NIU Ji-hui
Institution:1. Institute of Geologic Survey of ,lilin Province, Changchun 130061, China 2. Jilin Institute of Geological Sciences, Changchun 130012, China
Abstract:The Jingushan Au deposit occurred in the Kedao Formation strata, the mineralizing type belongs to structural altered rock one. The intermediate acidity volcano --clastic rock series formed by volcanic eruption and sedimentation is a basic factor and source bed for gold- forming, metamorphic deformation is a basic factor for gold-forming, vein rock action is a superimposed factor for gold--forming. The ore bodies were controlled by ductile shear metamorphic deformation belt, the genesis of the deposit is a superimposed compound one by metamorphic hydrothermal process and magmatic hydrothermal process.
Keywords:gold deposit  geologic features  discussion for genesis  Longjing of Jilin Province
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