| 于仕祥,姚良德,李厚民,赵洪振,洪学宽,杨志辽.鞍山陈台沟铁矿地质地球物理找矿模型[J].地质找矿论丛,2013,28(3):361-365 |
| 鞍山陈台沟铁矿地质地球物理找矿模型 |
| Geologic-geophysical exploration model of Chentaigou iron deposit in Anshan area |
| 投稿时间：2013-05-20 |
| DOI：10.6053/j.issn.1001-1412.2013.03.005 |
| 中文关键词: 陈台沟铁矿床 控矿地质条件 磁异常 地质-地球物理找矿模型 辽宁省 |
| 英文关键词:Chentaigou iron deposit ore-controllingconditions magnetic anomaly geologic-geophysical model Anshan area Liaoning province |
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| 摘要点击次数: 1916 |
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| 中文摘要: |
| 陈台沟铁矿床为新太古代时期形成的鞍山式沉积变质型铁矿床,是近年来在鞍山地区将地质与物探相结合,寻找深部贫铁矿床最为成功的典型范例。文章分析了陈台沟铁矿床的控矿地质条件及磁异常特征,建立了地质-地球物理找矿模型,对深部铁矿赋存部位进行了预测,并实施了钻探验证,以期为类似条件下寻找深部隐伏铁矿提供参考。 |
| 英文摘要: |
| Chentaigou iron deposit is an Neo-archean Anshan style sedimentary-metamorphic iron deposit. It is a typical successful example discovered to depth by integration of geological survey and geophysical survey. In order to provide reference for discovery blind iron deposit in areas with similar geological condition iron ore control conditions, magfnetic anomly characteristics, geological-geophysical ore-searching model, location prediction of iron ore to depth and dilling data of the deposit are analyzed and summarized in the paper. |
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