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Abstract:
亚拉坡金矿床位于位于甘河断裂破碎带的南侧,金矿主要赋存于蚀变基性岩内,为一中型金矿床。本文拟通过对矿区的区域、矿床地质特征进行初步研究,特别在对矿石氧化带及类型特征量做了进一步工作的基础上初步总结了矿区的矿床成因。
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中国机械
ISSN: 1003-0085
CN: 11-5417/TH
Year: 2014
Issue: 5
Page: 210-212
Cited Count:
SCOPUS Cited Count:
ESI Highly Cited Papers on the List: 0 Unfold All
WanFang Cited Count: -1
Chinese Cited Count:
30 Days PV: 2
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