| 新疆萨热克铜多金属矿成矿预测方法 |
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| 引用本文： | 贾润幸,方维萱,王磊,刘增仁,叶雷,李胜强.新疆萨热克铜多金属矿成矿预测方法[J].矿产勘查,2016,7(6):965-970. |
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| 作者姓名： | 贾润幸 方维萱 王磊 刘增仁 叶雷 李胜强 |
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| 作者单位： | 有色金属矿产地质调查中心,北京 100012,有色金属矿产地质调查中心,北京 100012,有色金属矿产地质调查中心,北京 100012,有色金属矿产地质调查中心,北京 100012,有色金属矿产地质调查中心,北京 100012,新疆鑫汇矿业有限公司,乌鲁木齐 830011 |
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| 基金项目： | 中国地质调查局项目(编号:12120114081501)和国土资源部公益性行业科研专项项目(编号:201511016)联合资助。 |
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| 摘 要： | 对于沉积盆地中的面状矿化体,在研究其成矿规律的前提下,通过对萨热克铜多金属矿以往钻探成果资料的综合整理,基于GIS平台圈定了萨热克铜多金属矿的空间分布形态,主要包括矿体厚度等值线图、成矿强度等值线图、矿体上盘厚度等值线图、矿体下盘厚度等值线图,遵循从已知到未知的找矿方法,可大大提高成矿预测的效果。
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| 关 键 词： | 成矿强度 成矿预测 砂砾岩型 萨热克铜多金属矿 新疆 |
| 收稿时间： | 3/4/2016 12:00:00 AM |
Mineral prediction methods in Sareke copper polymetallic deposit, Xinjiang |
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| JIA Run-xing,FANG Wei-xuan,WANG Lei,LIU Zeng-ren,YE Lei and LI Sheng-qiang.Mineral prediction methods in Sareke copper polymetallic deposit, Xinjiang[J].Mineral Exploration,2016,7(6):965-970. |
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| Authors: | JIA Run-xing FANG Wei-xuan WANG Lei LIU Zeng-ren YE Lei and LI Sheng-qiang |
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| Affiliation: | China Non-ferrous Metals Resource Geological Survey, Beijing 100012,China Non-ferrous Metals Resource Geological Survey, Beijing 100012,China Non-ferrous Metals Resource Geological Survey, Beijing 100012,China Non-ferrous Metals Resource Geological Survey, Beijing 100012,China Non-ferrous Metals Resource Geological Survey, Beijing 100012 and Xinjiang Xinhui Mineral Corporation, Urumqi 830011 |
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| Abstract: | For planar mineralized bodies in sedimentary basin, the spatial shape of Sareke copper polymetallic orebodies can be delineated on GIS platform based on integrated analysis of previous drilling data and study result on the metallogenic regularity, such as ore body thickness isogram map, ore-forming intensity isogram map, hangingwall thickness isogram map and footwall thickness isogram map etc.. These isogram maps and comprehensive research result can predict the unknown ore body from the known orebody and greatly improve the prospecting effect. |
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| Keywords: | ore-forming intensity mineral prediction glutenite type Sareke copper polymetallic deposit Xinjiang |
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