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GUO Zehua, WANG Lei, HAN Runsheng, CHEN Xinglin, BAI Longan. 2019. Tectonic geochemical characteristics and ore prediction in Hongdoushan copper deposit, Yunxian area, Western Yunnan[J]. Geology in China, 46(1): 178-190. doi: 10.12029/gc20190111
Citation: GUO Zehua, WANG Lei, HAN Runsheng, CHEN Xinglin, BAI Longan. 2019. Tectonic geochemical characteristics and ore prediction in Hongdoushan copper deposit, Yunxian area, Western Yunnan[J]. Geology in China, 46(1): 178-190. doi: 10.12029/gc20190111
shu

Tectonic geochemical characteristics and ore prediction in Hongdoushan copper deposit, Yunxian area, Western Yunnan

  • 1.

    Kunming University of Science and Technology, Southwest China Geological Survey, Geological Survey Center for Non-ferrous Mineral Resources, Kunming 650093, Yunnan, China

  • 2.

    Datun Coal Electricity Corp of China Coal Energy Group, Peixian 221611, Jiangsu, China

  • 3.

    Beijing Huayusheng Minerals Investment Co., Ltd., Yunxian 675800, Yunnan, China

    • Fund Project: Supported by National Natural Science Foundation (No.41762010, 41202069), Science and Technology Plan Foundation Projects in Yunnan Province (No. 2014FB122), School Enterprise Cooperation Project (No. 20130039), Projects for Yunnan Engineering Laboratory of Mineral Resources Prediction and Evaluation (YM lab) (2010) and Yunnan, school Innovation Team(2009, 2012)
More Information
  • Author Bio: GUO Zehua, male, born in 1992, master candidate, majors in mineral exploration and exploration; E-mail:903065518@qq.com
  • Corresponding author: WANG Lei, male, born in 1983, doctor, associate professor, major in the study of ore deposit and metallogenic prediction; E-mail:120901163@qq.com 
Received Date:  15 November 2017
Revised Date:  21 May 2018
Publish Date:  25 February 2019
    Abstract

  • This paper systematically summarizes the mineralization conditions of the volcanic arc metallogenic belt in southern Lancang River and the geological features of the Hongdoushan ore district. The authors studied the tectonic geochemistry at 1272 and 1220 level. On the basis of the analysis of the data collected from tectonic rock samples and by means of R-type cluster analysis and factor analysis, the authors delineated combinational anomalies of mineralization elements. The authors found that the distribution of anomalies in the altered rock is controlled by NE-trending F1 fracture and NWW-EW-trending F3 fracture in the mining area. The zonation of high temperature and low temperature anomalies occur successively from fracture to surrounding rock, indicating the direction of fluid migration as well as the information of orebodies and provided evidence for deep ore prediction. Through the researches on structural ore-controlling regularity and tectonic geochemistry, the authors found the occurrence and deep extension of the NE-trending orebody, delineated the orebodies controlled by NWW-and nearly EW-trending fractures at the 1272 level. Field work demonstrated favorable ore-prospecting areas in the anomaly distribution zone and deep prediction target area, the copper orebody was delineated and predicted, which extends stably to the depth. The authors estimate that the resource reserves are about 50, 000 tons. The magmatic hydrothermal orebody controlled by tectonics has the prospect of reaching the medium copper deposit.

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