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J4 ›› 2007, Vol. 15 ›› Issue (6): 30-34.
• 矿产勘查 • 上一篇 下一篇
杨银成,周金玺,彭勇,沈刚刚
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作者简介:
YANG Yincheng,ZHOU Jinxi,PENG Yong,SHEN Ganggang
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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:
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.
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链接本文: http://www.goldsci.ac.cn/CN/
http://www.goldsci.ac.cn/CN/Y2007/V15/I6/30
[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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