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| Potentiality assessment of mineral resources from Heiqia to Sanshiliyingfang in West Kunlun area |
| YANG Chen1,2, WANG Hui1, ZHANG Shaopeng1, LIAO Youyun1, LIU Huan1 |
1. Geological Exploration Institute of Aerial Photogrammetry and Remote Sensing Bureau, Xi’an 710199, China;
2. State Key Laboratory for Continental Dynamics, Northwest University, Xi’an 710069, China |
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Abstract According to the 1∶50,000 stream sediments survey, large scale mineral geological mapping, geochemical comprehensive profile and exploratory trench in Heiqia to Sanshiliyingfang areas of West Kunlun, the authors evaluated the prospecting potential based on the geological characteristics of minerals, metallogenic types and prospecting rules in this region.The research indicates that there are three main types of deposits in this area: submarine exhalative-sedimentation (remold) type iron polymetallic ore in Heqia sea, marine sedimentary type of iron ore containing titanium in southern Atake river and stratum-controlled copper gold mine in northern Atake river. Seven metallogenic prediction regions were identified, including one class A, one class B, and five class C areas. The estimated resources were 15.656 9 million tons of iron ore, 0.397 3 million tons of manganese ore, 3.5 thousand tons of copper, 13.3 thousand tons of lead metal, 25.8 thousand tons of zinc and 0.147 6 million tons of titanium. Five prospecting target areas were further delineated, including two class A and three class B target areas. The authors also suggested that priority should be given to the prospecting work of Fe, Pb and Zn in the iron polymetallic mineralization belt of Heiqia in order to further expand the prospecting results. This marine sedimentary type iron ore containing titanium was first discovered in Early Carboniferous group, which is expected to achieve significant prospecting breakthrough.
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Received: 18 April 2018
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[1] 中国科学院青藏高原综合科学考察队.喀喇昆仑山—昆仑山地区地质演化[M].北京:科学出版社,2000.
[2] 姜春发,王宗起,李锦轶.中央造山带开合构造[M].北京:地质出版社,2000.
[3] 潘桂棠,李兴振,王立全,等.青藏高原及邻区大地构造单元初步划分[J].地质通报,2002,21(11):701-707.
[4] 许志琴,李思田,张建新,等.塔里木地块与古亚洲/特提斯构造体系的对接[J].岩石学报,2011,27(1):1-22.
[5] 韩芳林. 西昆仑增生造山带演化及成矿背景[D].北京:中国地质大学(北京),2006.
[6] 李文渊,董福辰,张照伟,等.西北地区矿产资源成矿远景与找矿部署研究主要进展及成果[J].中国地质调查,2015,2(1):18-24.
[7] 校培喜,高晓峰,康磊,等.西昆仑—阿尔金成矿带地层-岩石-构造时空格架及成矿地质背景新认识[J].中国地质调查,2015,2(2):48-55.
[8] 杨金中,王海庆,陈微.西昆仑成矿带高分辨率遥感调查主要进展与成果[J].中国地质调查,2016,3(5):7-12.
[9] 李荣社,计文化,杨永成,等.昆仑山及邻区地质[M].北京:地质出版社,2008:1-5.
[10] 乔耿彪,伍跃中,杨合群.新疆西昆仑地区各成矿单元地质特征及找矿方向[C]//中国地质学会2013年学术年会论文摘要汇编.北京:中国地质学会,2013:103-108.
[11] 王辉,杨晨,张少鹏,等.西昆仑成矿带黑恰至三十里营房地区矿产地质调查报告[R].2015.
[12] 中国地质调查局.1∶50 000矿产地质调查工作指南(试行)[R].北京:中国地质调查局,2016. |
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2018, Vol. 5 
