摘要
大台沟铁矿位于本溪市南郊桥头镇,距本溪市约16 km。矿床属前寒武纪硅铁质建造。通过对矿床的成矿作用、矿床地质特征的分析,提出了大台沟铁矿床的成矿机制、矿体形态、矿物共生组合、围岩蚀变等方面的矿化特征,部分揭示了大台沟铁矿床的成矿模式及找矿标志。
Dataigou iron ore deposit lies in bridge town of Benxi city, which is about 16 km away from Benxi city. The ore deposit belongs to ferrosilicon geology structure during the precambrian period. By the analysis of the metallogenesis and the geological feature, the mineralization features of ore body shape, mineral symbiotic combination, and wall rock alteration are proposed. It reveals the metallogenic model of Dataigou iron ore deposit and the prospecting marks.
出处
《辽宁科技大学学报》
CAS
2010年第4期353-355,共3页
Journal of University of Science and Technology Liaoning
关键词
铁矿
鞍山式铁矿
成因
找矿标志
iron mine
Anshan iron deposit
cause
prospecting marks
