青海省肯德可克金矿热水沉积层矽卡岩特征及成矿意义

高章鉴; 罗才让; 井继锋

青海省肯德可克金矿热水沉积层矽卡岩特征及成矿意义

西北有色地质研究所, 陕西西安 710054

基金项目: 中国有色金属工业总公司重点找矿科研项目资助(项目编号96-D-24)

收稿日期: 2000-08-07

修回日期: 2001-05-06

刊出日期: 2001-06-15

Features and mineralization significance of stratiform skarns of hydrothermal fluid sedimentary origin in Kendekoke gold deposit, Qinhai

Institute of Geology, Chinese Northwest Geoexploration Norferrous Bureau, Xi'an 710054, China

Received Date: 07 August 2000

Revised Date: 06 May 2001

Publish Date: 15 June 2001

摘要

摘要: 热水沉积成因层矽卡岩在青海省肯德可克金矿区非常发育。其产出特征、结构、构造及与岩体的关系等与接触交代型矽卡岩都有显著的区别。层矽卡岩是该区金矿化主要控矿因素之一,同时也是重要区域找矿标志。
- 热水沉积 /
- 层矽卡岩 /
- 肯德可克金矿 /
- 祁漫塔格 /
- 青海
Abstract: The stratiform skarns of hydrothermal fluid sedimentary origin are well developed in Kendekoke gold deposit,Qinhai province.And their development features,textures,structures and the relation with magma intrusion are obviously different from the skarns of contact metasometic origin type.The stratiform skarn is a major factor of gold mineralization control and the regional ore-searching criteria.
- Hydr othermal fluid sediment /
- stratiform skarns /
- Kendekoke gold deposit /
- Qinhai /

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参考文献(5)

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李福东,张汉文,等.鄂拉山地区热水成矿模式--以铜为主多金属[M].西安:西北大学出版社,1993.

Stanton R L.Constitutional features and some exploration implications of three zinc-bearing stratiform skarns of eastern Australia[C].Trans Instn Min Metall (Sect B:Appl Earth Sci).1986,96:B37-B57.

Einaudi M T. Skans deposits[J].Economic Geology Seventy-Fifth Anniversary Volume,1981.

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青海省肯德可克金矿热水沉积层矽卡岩特征及成矿意义

西北有色地质研究所, 陕西 西安 710054

Features and mineralization significance of stratiform skarns of hydrothermal fluid sedimentary origin in Kendekoke gold deposit, Qinhai

Institute of Geology, Chinese Northwest Geoexploration Norferrous Bureau, Xi'an 710054, China

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西北有色地质研究所, 陕西西安 710054