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Application of induced polarization method in antimony ore exploration of Dachang in Guizhou |
ZHANG Xijun1,2, LI Jiabin1,2, MENG Yinghua1,2, QU Niannian1,2 |
1. Guizhou Institute of Geological Survey, Guiyang 550081, China 2. Guizhou Engineering Research Center for Geologic-Geophysical Exploration Development and Application, Guiyang 550081, China |
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Abstract This paper briefly introduced the basic theory and working methods of induced polarization (IP) method, and the geological and geophysical characteristics of Dachang antimony ore area in Guizhou. The application effect of IP method in antimony ore exploration was mainly discussed. Through comprehensive analysis and research on anomaly of IP intermediate gradient and IP sounding,the authors attained the spatial variation characteristics of strata resistivity in the study area. Then the strata boundary between the Mount Emei basalt and Longtan sandstone was identified. The structure of the study area was deduced and the ore bearing favorable position was circled. Comparing with the drilling data, the authors found that the geophysical exploration and the drilling data were basically consistent, which indicated that IP has good antimony ore prospecting results(IP).
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Received: 23 March 2017
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[1] 王金贵,张鑫全,李典,等.综合方法在内蒙古杭盖音浑迪浅覆盖区寻找隐伏矿床中的应用[J].中国地质调查,2016,3(4):69-75. [2] 周德忠,杨国桢,毛健全.贵州晴隆大厂火山沉积-构造改造锑矿床地质特征及成因分析[J].贵州工学院学报,1980,9(1):1-18. [3] 陈豫,刘秀成,张启厚.贵州晴隆大厂锑矿床成因探讨[J].矿产地质,1984,3(3):1-12. [4] 张启厚,黄华斌,戎昆方.贵州晴隆大厂锑矿床古喀斯特层滑构造与成矿关系的初步讨论[J].贵州工学院学报,1989,18(4):43-49. [5] 孙跃,杨少平,袁桂琴,等.地质调查技术方法信息网中物化探技术方法库内容建设[J].中国地质调查,2015,2(5):56-62. [6] 廖善友,胡涛.贵州晴隆大厂锑矿床控矿条件及成矿机制[J].贵州地质,1990,7(3):229-236. [7] 韦天姣.贵州锑矿地质勘查与研究的进展[J].贵州地质,1991,8(1):23-31. [8] 夏勇,张启厚,黄华斌.大厂锑矿田构造控矿特征及实验构造地球化学初步研究[J].地质与勘探,1993,29(10):48-53. [9] 刁理品,韩润生,刘鸿,等.贵州晴隆大厂锑矿地质及控矿因素[J].云南地质,2006,25(4):467-473. [10] 刁理品,韩润生,李波,等.黔西南晴隆大厂锑矿田构造控矿特征[J].昆明理工大学学报:理工版,2008,33(2):5-10. [11] 沈忠义,胡煜昭,韩润生,等.贵州晴隆大厂锑矿田固路锑矿床控矿因素分析[J].矿产与地质,2010,24(4):294-299. [12] 张西君,蒙应华,屈念念,等.贵州省晴隆县大厂矿集区找矿预测物探工作报告[R].贵阳:贵州省地质调查院,2016. |
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