Discussion about Geological Characteristics and Genesis of an Au-polymetal Deposit in Sichuan Province

饶玉彬; 陈富贵

doi:10.16056/j.1005-7676.2015.04.012

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Discussion about Geological Characteristics and Genesis of an Au-polymetal Deposit in Sichuan Province

更新时间：2026-01-19

- Discussion about Geological Characteristics and Genesis of an Au-polymetal Deposit in Sichuan Province
- Issue 4, Pages: 44-46(2015)
- 作者机构：
  
  江西省煤田地质勘察研究院
- 作者简介：
- 基金信息：
- DOI：10.16056/j.1005-7676.2015.04.012
  CLC： P618.2
- Published：2015
- 稿件说明：
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[1]饶玉彬,陈富贵.四川某金多金属矿床地质特征及成因探讨[J].能源研究与管理,2015(04):44-46.

饶玉彬, 陈富贵. Discussion about Geological Characteristics and Genesis of an Au-polymetal Deposit in Sichuan Province[J]. 2015, (4): 44-46.
[1]饶玉彬,陈富贵.四川某金多金属矿床地质特征及成因探讨[J].能源研究与管理,2015(04):44-46. DOI： 10.16056/j.1005-7676.2015.04.012.

饶玉彬, 陈富贵. Discussion about Geological Characteristics and Genesis of an Au-polymetal Deposit in Sichuan Province[J]. 2015, (4): 44-46. DOI： 10.16056/j.1005-7676.2015.04.012.

摘要

该金多金属矿床赋存于花岗岩过渡相及边缘相部位

主要受断裂构造控制;矿脉形态为豆荚状及脉状

与围岩接触界线清楚

呈突变过渡;矿石中金粒结晶微细

扩散交代作用微弱

金属矿物多属中温矿物;其矿床成因类型隶属中温热液充填型矿床

产出地质特征分类应属破碎带蚀变岩型金矿床。

Abstract

The Au-polymetal deposit occurs in granite transitional facies and marginal facies

mainly controlled by fracture structure. The pattern of Vein is the podiform and vein

contact with the surrounding rock boundaries clear

showed by mutation transition. Gold grains with fine crystallization In the ore

diffusion metasomatism is weak

metal minerals are medium temperature. The genetic types of ore deposits belong to the warm liquid filling type deposit. Geological characteristics of classification should be belong to the gold deposit of alteration rock type in the fracture zone.

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