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[an error occurred while processing this directive]Application of High Density Electrical Method in Prospecting for Duoguma Antimony Gold Ore Spot in North Bayan Har Mountains
Received date: 2021-12-28
Revised date: 2022-03-29
Online published: 2022-10-31
In order to solve the problem that restrict the breakthrough of prospecting(such as ore controlling factors and deposit genesis) in Duoguma antimony gold mining area, the 1∶200 000 As乙 41Sb (Au) stream sediment anomaly and 1∶50 000 Au、As、Sb stream sediment anomaly in Duoguma area of Maduo County were examined by high-density electrical method, and the North Duoguma antimony gold mining point and its periphery were mainly detected.The plane resistivity anomaly shows that the regional NW trending Kunlun Mountain pass Maduo-Gande-Jiuzhi fault is transformed by the later NE trending fault dislocation in this area.High value charge rate (polarizability) anomalies are superimposed at the intersection of the two groups of fault structures. The long axis direction of these anomalies is consistent with the trend of regional structure, and the location is mainly distributed on the side of structural tendency.Combined with the analysis of resistivity section anomalies, these widely distributed and strong anomalies are mainly distributed in the contact zone between regional structure and surrounding rock. The charging rate (polarizability) anomaly combined with the anomaly of polymetallic elements such as antimony and gold in geochemical exploration is selected as the prospecting target for engineering verification.The antimony gold orebody is revealed through trenching engineering, realizing the prospecting breakthrough of the polymetallic prospecting target.
Dexi MA , Xirong REN , Jiong SONG , Baowei ZHANG . Application of High Density Electrical Method in Prospecting for Duoguma Antimony Gold Ore Spot in North Bayan Har Mountains[J]. Gold Science and Technology, 2022 , 30(4) : 498 -507 . DOI: 10.11872/j.issn.1005-2518.2022.04.009
http://www.goldsci.ac.cn/article/2022/1005-2518/1005-2518-2022-30-4-498.shtml
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|
|
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|
|
|
|
|
|
白国典,何凯,琚根社,等,2018.区域化探成果在青海北巴颜喀拉山地区地质填图中的应用[J].物探与化探,42(3):429-435.
|
|
包存义,许国五,李玉春,等,2003.大场地区金矿成因类型及成矿潜力分析[J].青海国土经略,3(3):17-22.
|
|
陈守建,李荣社,计文化,等,2011.巴颜喀拉构造带二叠—三叠纪岩相特征及构造演化[J].地球科学—中国地质大学学报,26(3):394-405.
|
|
韩英善,2009.青海省北巴颜喀拉山金矿成矿环境及预测研究[R].西宁:青海省第三地质矿产勘查院.
|
|
李琳业,俞长捷,戴梅芳,等,2009.青海省大场金矿床地质特征及找矿远景分析[J].青海大学学报,27(1):12-16.
|
|
李学虎,2017.青海省夺尔贡玛锑矿区地质和勘查地球化学特征分析[D].西安:长安大学.
|
|
梁超,李学虎,任永吉,2015.青海北巴颜喀拉地区金矿地质特征及成矿规律[J].中国科技纵横,(23):183-185.
|
|
强晓农,2019.青海北巴金成矿带西段藏金沟金锑矿地质、地球化学特征及成矿预测[D].长春:吉林大学.
|
|
宋志俭,王玉德,李发业,等,2005.青海省曲麻莱县大场金矿外围1∶5万化探普查报告[R].西宁:青海省地质调查院.
|
|
杨欣德,鄢犀利,2011.青海达日—久治地区巴颜喀拉盆地研究进展[J].地质力学学报,17(1):79-85.
|
|
袁万明,莫宣学,喻学惠,等,2000.东昆仑热液金成矿带及其找矿方向[J].地质与勘探,36(5):20-23.
|
|
赵俊伟,孙丰月,李世金,等,2007.青海北巴颜喀拉山地区浊积岩中金(锑)矿成矿地质特征——以大场一加给陇洼一带为例[J].黄金,3(9):8-13.
|
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