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川西铜炉房造山型金矿床成因:基于矿物学、流体包裹体和热力学模拟的证据

周春波 梁翼 葛行飞 屈尚伦 沈开红 徐勇 刘洋 黄皓南 角兴宇 裴秋明

成都理工大学学报(自然科学版)2025,Vol.52Issue(4):253-269,17.
成都理工大学学报(自然科学版)2025,Vol.52Issue(4):253-269,17.DOI:10.12474/cdlgzrkx.2024011902

川西铜炉房造山型金矿床成因:基于矿物学、流体包裹体和热力学模拟的证据

Ore genesis of the Tonglufang orogenic gold deposit in western Sichuan:Constraints from mineralogy,fluid inclusions,and thermodynamic simulations

周春波 1梁翼 2葛行飞 2屈尚伦 3沈开红 1徐勇 1刘洋 1黄皓南 2角兴宇 2裴秋明2

作者信息

  • 1. 四川省地球物理调查研究所,成都 610032
  • 2. 西南交通大学 地球科学与环境工程学院,成都 611756
  • 3. 康定市自然资源局,四川 康定 626000
  • 折叠

摘要

Abstract

The Tonglufang gold deposit is located in the southwestern part of the Songpan-Ganzi orogenic belt,in the Guza-Kongyu-Danba gold metallogenic province.Gold-bearing ores in the Tonglufang deposit are mainly found in pyrite-rich quartz veins,sulfide-rich quartz veins,and malachite/limonite-rich quartz veins.Based on a field investigation and microscope analysis,the gold mineralization is divided into two stages:(Ⅰ)a quartz-gold-pyrite stage and(Ⅱ)a quartz-gold-polymetallic sulfide stage.In this paper,the genetic types and mineralization characteristics of the Tonglufang gold deposit are analyzed by means of electron probe microanalysis(EPMA),fluid inclusion,laser ablation inductively coupled plasma mass spectrometry(LA-ICP-MS)mapping,and thermodynamic calculations.The microthermometric analysis of fluid inclusions reveals two homogenization temperature peaks(300~320℃and 360~380℃)and two salinity(NaCleqv)peaks(8%~10%and 12%~14%),indicating low to intermediate temperature and salinity in the ore-forming,H2O-NaCl-CO2-type fluid.The LA-ICP-MS mapping analysis shows that the contents of trace elements including As,Au,Ag,Cu,Pb,Zn,Co,Ni,Bi,and Sb are much higher in the pyrite at stage Ⅰ than those at stage Ⅱ,while the Au/Ag ratios are low in the pyrite in both stages.The characteristics of the ore-forming fluids and mineral assemblages may indicate the Tonglufang deposit is an orogenic gold deposit,while the range of gold fineness and trace element composition of pyrite may indicate a mantle-fluid origin.

关键词

金成色值/流体包裹体/LA-ICP-MS/铜炉房金矿床/松潘—甘孜造山带

Key words

gold fineness/fluid inclusion/LA-ICP-MS/Tonglufang gold deposit/Songpan-Ganzi orogenic belt

分类

地质学

引用本文复制引用

周春波,梁翼,葛行飞,屈尚伦,沈开红,徐勇,刘洋,黄皓南,角兴宇,裴秋明..川西铜炉房造山型金矿床成因:基于矿物学、流体包裹体和热力学模拟的证据[J].成都理工大学学报(自然科学版),2025,52(4):253-269,17.

基金项目

国家自然科学基金项目(41702077) (41702077)

中央高校基本科研业务费专项资金(2682016CX090). (2682016CX090)

成都理工大学学报(自然科学版)

OA北大核心

1671-9727

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