青海省祁连县热水沟铁矿地质特征及成因探讨

J4 ›› 2007, Vol. 15 ›› Issue (6): 30-34.

青海省祁连县热水沟铁矿地质特征及成因探讨

杨银成，周金玺，彭勇，沈刚刚

青海省有色地质矿产勘查院，西宁810007

收稿日期:2007-08-28 修回日期:2007-10-15 出版日期:2007-12-28 发布日期:2011-09-02
作者简介:杨银成(1963-)，男，工程师，主要从事铜、金等有色金属勘查.

Geological Characteristics and Original Discussion of Eastern Reshuigou Iron Deposit in Qilian County，Qinghai

YANG Yincheng，ZHOU Jinxi，PENG Yong，SHEN Ganggang

Geology and Mineral Exploration Institute，Qing Hai Provincal Bureau Geology and Mineral Exploration，Xi Ning 810007，China

Received:2007-08-28 Revised:2007-10-15 Online:2007-12-28 Published:2011-09-02

摘要/Abstract

摘要：

热水沟铁矿矿体主要受早奥陶世阴沟群地层控制，其成因为火山—沉积变质矿床，找矿标志为早奥陶世阴沟群及矿区内磁异常。

关键词: 铁矿床, 基本特征, 矿床成因, 找矿标志, 热水沟

Abstract:

The Iron ore at east Reshuigou is mainly controlled by the stratum of Yingouqun which form early ordovician epoch，the stratum is a condition to find The iron ore there．And another condifion is abnormality of magnetism．The Iron 0re form for volcanic-deposit metamorphose．

Key words: iron deposit, essential features, cause of deposit formation, condition of finding ore, Reshuigou

中图分类号:

P618.01/P618.31

杨银成，周金玺，彭勇，沈刚刚. 青海省祁连县热水沟铁矿地质特征及成因探讨[J]. J4, 2007, 15(6): 30-34.

YANG Yincheng，ZHOU Jinxi，PENG Yong，SHEN Ganggang. Geological Characteristics and Original Discussion of Eastern Reshuigou Iron Deposit in Qilian County，Qinghai[J]. J4, 2007, 15(6): 30-34.

参考文献

[1] 翟裕生．古陆边缘成矿系统
[M]．北京：地质出版社，2002．

[2] 甘肃省地质局第二区域地质测量队．J-47-Ⅸ1/20万区调报告(内部资料)．1974．

[3] 杨银成、李宏录．青海省祁连县热水沟铁矿普查报告(内部资料)．西宁：青海省有色地质矿产勘查院，2004．

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