辽东白云-小佟家堡子矿集区控矿构造及成矿有利区预测

张拴宏; 胡国辉; 李建锋; 肖昌浩; 刘向冲; 张琪琪; 姚晓峰; 刘福兴; 王伟; 陈正乐; 张青

doi:10.3799/dqkx.2020.246

Volume 45 Issue 11

Nov. 2020

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Article Navigation > Earth Science > 2020 > 45(11): 3885-3899

Zhang Shuanhong, Hu Guohui, Li Jianfeng, Xiao Changhao, Liu Xiangchong, Zhang Qiqi, Yao Xiaofeng, Liu Fuxing, Wang Wei, Chen Zhengle, Zhang Qing, 2020. Ore-Controlling Structures and Metallogenic Favorable Area Prediction in Baiyun-Xiaotongjiabuzi Ore Concentration Area, Eastern Liaoning Province. Earth Science, 45(11): 3885-3899. doi: 10.3799/dqkx.2020.246

Citation:

Zhang Shuanhong, Hu Guohui, Li Jianfeng, Xiao Changhao, Liu Xiangchong, Zhang Qiqi, Yao Xiaofeng, Liu Fuxing, Wang Wei, Chen Zhengle, Zhang Qing, 2020. Ore-Controlling Structures and Metallogenic Favorable Area Prediction in Baiyun-Xiaotongjiabuzi Ore Concentration Area, Eastern Liaoning Province. Earth Science, 45(11): 3885-3899. doi: 10.3799/dqkx.2020.246

Citation:

Zhang Shuanhong, Hu Guohui, Li Jianfeng, Xiao Changhao, Liu Xiangchong, Zhang Qiqi, Yao Xiaofeng, Liu Fuxing, Wang Wei, Chen Zhengle, Zhang Qing, 2020. Ore-Controlling Structures and Metallogenic Favorable Area Prediction in Baiyun-Xiaotongjiabuzi Ore Concentration Area, Eastern Liaoning Province. Earth Science, 45(11): 3885-3899. doi: 10.3799/dqkx.2020.246

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Ore-Controlling Structures and Metallogenic Favorable Area Prediction in Baiyun-Xiaotongjiabuzi Ore Concentration Area, Eastern Liaoning Province

doi: 10.3799/dqkx.2020.246

Zhang Shuanhong^{1, 2
,
,},
Hu Guohui^{1, 2},
Li Jianfeng^{1, 2},
Xiao Changhao^{1, 2},
Liu Xiangchong^{1, 2},
Zhang Qiqi^{1, 2},
Yao Xiaofeng³,
Liu Fuxing⁴,
Wang Wei⁴,
Chen Zhengle^{1, 2},
Zhang Qing^{1, 2}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China
3.
Development and Research Center, China Geological Survey, Beijing 100037, China
4.
103 Branch of Non-Ferrous Geological Bureau of Liaoning Province, Dandong 118008, China

Received Date: 2020-07-19
Publish Date: 2020-11-15

Abstract

Abstract

The Baiyun-Xiaotongjiabuzi ore concentration area is one main part of the Qingchengzi ore concentration areas in eastern Liaoning Province. It consists of Baiyun (Erdaogou,Sandaogou) and Huangdianzi gold ore deposits in the north and Linjiasandaogou,Xiaotongjiabuzi,Yangshu,Taoyuan gold ore deposits and Gaojiabuzi,Fengyindadi and Jiangjiagou Ag ore deposits in the south. The results show that the Baiyun (Erdaogou,Sandaogou) and Huangdianzi gold ore deposits in the north are controlled by east-west striking thrust fault system that is about 8 km long along its strike. The ore-hosting thrust fault system dips to south with an average dipping angle of 30°. It is composed of a main thrust fault and several paralleling thrust faults and is about 200 m wide. The main thrust fault cut through the foliations of Dashiqiao and Gaixian formations and other paralleling thrust faults are usually developed along foliations of Dashiqiao and Gaixian formations. The thrust faults are characterized by wave-like surface and the thrust surfaces with low angle are favorable areas for ore bodies. The Linjiasandaogou,Xiaotongjiabuzi,Yangshu,Taoyuan gold ore deposits and Gaojiabuzi,Fengyindadi and Jiangjiagou Ag ore deposits in the south are controlled by north-dipping low angle thrust fault. The ore-hosting thrust faults are developed near the contacts between the metaclastic rocks of Gaixian Formation and marbles of Dashiqiao Formation. Gold and Pb-Zn-Ag ore bodies exist within the thrust faults developed in the metaclastic rocks and marbles,respectively. The NW striking Jianshanzi fault is the largest and high angle fault in the area with a length over 13 km. Field investigation and kinematic analysis results show that the Jianshanzi fault is a multi-stage fault and served as dextral strike-slip in early stage and normal fault in late stage. After formation of the main gold and Pb-Zn-Ag ore deposits in the Baiyun-Xiaotongjiabuzi ore concentration area during the Triassic period,the Jianshanzi fault exhibited strong dextral strike-slip movement and the east-west striking ore-hosting thrust fault system in Baiyun-Huangdianzi ore deposits in west side of the Jianshanzi fault was most likely moved 6 km to south to the Hujiabuzi-north Maweizi-Maodianzi area in east side of the Jianshanzi fault. Based on the analysis results on the ore-controlling structures,ore-bearing strata and movements of the post-metallogenic faults,it is proposed south Baiyun-Huangdianzi ore deposits and Xiaotongjiabuzi-Fengyindadi as two deep metallogenic favorable areas,and Hujiabuzi-north Maweizi-Maodianzi and South Taoyuan village as two outside metallogenic favorable areas.

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Ore-Controlling Structures and Metallogenic Favorable Area Prediction in Baiyun-Xiaotongjiabuzi Ore Concentration Area, Eastern Liaoning Province

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