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贵州灰家堡金矿田成矿与蚀变元素迁移

赵廷严 董树义 程文斌 李葆华 公凡影 刘鹏 李永玲 王洋 刘琳琳

成都理工大学学报(自然科学版)2017,Vol.44Issue(4):494-505,12.
成都理工大学学报(自然科学版)2017,Vol.44Issue(4):494-505,12.DOI:10.3969/j.issn.1671-9727.2017.04.13

贵州灰家堡金矿田成矿与蚀变元素迁移

Study on mineralization and migration of alteration elements in Huijiabao gold field, southwestern Guizhou, China

赵廷严 1董树义 2程文斌 2李葆华 2公凡影 3刘鹏 4李永玲 5王洋 6刘琳琳7

作者信息

  • 1. 中国国土资源航空物探遥感中心,北京100083
  • 2. 成都理工大学 地球科学学院,成都610059
  • 3. 中国地质调查局 发展研究中心,北京100037
  • 4. 国土资源部 矿产勘查技术指导中心,北京100120
  • 5. 北京超图软件股份有限公司,北京100015
  • 6. 黑龙江省有色金属地质勘查七○七队,黑龙江绥化152054
  • 7. 贵州省有色金属和核工业地质勘查局七总队,贵阳550005
  • 折叠

摘要

Abstract

The Shuiyindong deposit and Taipingdong deposit in the Huijiabao ore field are selected to study the migration regularity and mode of elements in the process of wallrock alteration of the Carlin-type gold deposit and to explore the internal relationship between the alteration and gold mineralization.Study of typical surrounding rocks,mineralization rocks,ore petrographic characteristics and corresponding grant mass balance equation shows that the type of wallrock alteration corresponding to the metallogenic stage of the Carlin-type gold deposit is consistent with the element migration law revealed by calculation.Geochemical thermodynamics calculation suggests that gold mainly migrates in the form of AuHS0 complex in the ore-forming solution.It shows that the wallrock alteration in different metallogenic stages promotes the migration of major ore-forming materials in the Carlin-type gold deposits,and then precipitates and enriches the gold ore formation.

关键词

地球化学/元素迁移/金的迁移形式/围岩蚀变/灰家堡金矿田

Key words

geochemistry/element migration/migration of gold/wallrock alteration/Huijiabao gold orefield

分类

天文与地球科学

引用本文复制引用

赵廷严,董树义,程文斌,李葆华,公凡影,刘鹏,李永玲,王洋,刘琳琳..贵州灰家堡金矿田成矿与蚀变元素迁移[J].成都理工大学学报(自然科学版),2017,44(4):494-505,12.

基金项目

中国地质调查局地调项目(12120120300016006). (12120120300016006)

成都理工大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1671-9727

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