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The prediction and prospecting direction of polymetallic deposits in the Wutaishan-Hengshan area |
Sheng-Sheng XUE, Shuang-Kui ZHANG, Nan ZHAO, Xin-Peng ZHOU, Zhi-Bin JIN |
Shanxi Geophysical and Geochemical Exploration Institute,Yuncheng 044000,China |
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Abstract In this study, the moving average method was used to reprocess the 1∶200,000 stream sediments data from seven sheets in Wutaishan-Hengshan area. In combination with the 1∶200,000 gravity data and 1∶50,000 aeromagnetic data obtained in this area, the authors found that the comprehensive anomalies are in good agreement with the deposits related to the Yanshanian rock mass. Choosing elements such as Au, Ag, Cu, Pb, Zn anomalies and high-magnetic and low-gravity anomalies as the prediction criteria, the authors predicted a total of 13 polymetallic ore prospective areas related to the mineralization of rock masses in the study area. According to available data, there are 9 NW-trending fault structural zones in this area. The intrusive position of the rock mass is controlled by the intersection of the NW-trending fault and the NE-trending fault. Most of the known rock masses and the 11 prospective areas predicted by this paper are distributed in the fault structural belt, forming multiple tectonic magmatic zones. The polymetallic ore deposit is inextricably linked with Yanshanian rock mass.
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Received: 11 April 2018
Published: 20 February 2019
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Geological map of the Wutaishan-Hengshan area
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Anomalies of the Yixingzhai deposit a—geological sketch map; b—anomalies distribution of Cu-Pb-Au-Ag; c—anomalies distribution of Mo-Bi; d—gravity anomaly; e—magnetic anomaly
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Anomalies of the Diaoquan deposit a—geological sketch map; b—anomalies distribution of Cu-Pb-Zn-Au-Ag; c—anomalies distribution of W-Mo-Bi; d—gravity anomaly; e—magnetic anomaly
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参数 | 新生界 | 中生界 | 古生界 | 元古宇 | 太古宇 | 燕山期岩浆岩 | 吕梁期岩浆岩 | 五台期岩浆岩 | 密度/(g·cm-3) | 1.62~1.82 | 2.5 | 2.65 | 2.77 | 2.71 | 2.52~2.72 | 2.62~3.05 | 2.62~3.05 | 磁化率/(10-64πSI) | | | | 22 | 25~158 | 100~3366 | 79 | 112~377 |
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Physical parameter of stratum and magmatic rock in the Wutaishan-Hengshan area[23]
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编号 | 预测区 名称 | 位置 | 中低温元素 | 高温 元素 | 重力 异常 | 磁法 异常 | 备注 | 1 | 仲沟 | 繁峙 | Au、Ag、Pb、Zn | W、Mo、Bi | 梯度带 | 高磁 | 高中温元素套合程度高 | 2 | 招柏 | 灵丘 | Au、Ag、Pb、Zn | 无 | 低重 | 无异常 | 中低温元素套合程度较高 | 3 | 龙须台 | 灵丘 | Au、Ag、Pb、Zn、Cu | W、Mo | 低重 | 无异常 | 高中温元素套合程度非常高;银、锌异常范围广 | 4 | 虎头寨 | 灵丘 | Au、Ag、Pb、Zn、Cu | W、Bi | 梯度带 | 梯度带 | 高中温元素异常套合好;附近发育有砂金矿 | 5 | 龙王堂 | 应县 | Au、Ag、Pb | 无 | 弱低重 | 梯度带 | 中低温元素套合程度高 | 6 | 山岔 | 应县 | Au、Ag、Zn、Cu | 无 | 弱高重 | 无异常 | 异常套合较好 | 7 | 张旺 | 浑源 | Au、Ag、Pb | 无 | 低重 | 局部高磁 | 异常套合好 | 8 | 高庄 | 浑源 | Au、Zn、Pb | 无 | 低重 | 梯度带 | 异常套合好 | 9 | 南梁 | 五台 | Au、Ag、Pb、Zn、Cu | 无 | 梯度带 | 梯度带 | 中低温元素套合较好 | 10 | 小寺 | 浑源 | Au、Ag、Zn、Cu | Mo | 梯度带 | 高磁 | 中低温元素套合较好 | 11 | 庄里 | 盂县 | Au、Ag、Zn、Cu | Bi | 梯度带 | 不明显 | 中低温元素套合较好 | 12 | 梁家寨 | 盂县 | Au、Ag、Pb、Zn、Cu | 无 | 弱低重 | 不明显 | 中低温元素套合较好 | 13 | 陈家庄 | 盂县 | Au、Ag、Zn、Cu | W、Mo、Bi | 梯度带 | 不明显 | 中低温元素套合较好 |
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Geochemical exploration, gravity and magnetic method for delineating polymetallic ore prediction areas in the Wutaishan-Hengshan area
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2],[5]) ">
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Mesh fracture structure and prediction zone in the Wutaishan-Hengshan area (The base map is modified according to the literature[2],[5])
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