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QIU Gengen, FANG Hui, Lü Qinyin, PENG Yan. 2019. Deep electrical structures and metallogenic analysis in the north section of Wuyishan Mountains and its adjacent areas: Based on three-dimensional magnetotelluric sounding results[J]. Geology in China, 46(4): 775-785. doi: 10.12029/gc20190408
Citation: QIU Gengen, FANG Hui, Lü Qinyin, PENG Yan. 2019. Deep electrical structures and metallogenic analysis in the north section of Wuyishan Mountains and its adjacent areas: Based on three-dimensional magnetotelluric sounding results[J]. Geology in China, 46(4): 775-785. doi: 10.12029/gc20190408
shu

Deep electrical structures and metallogenic analysis in the north section of Wuyishan Mountains and its adjacent areas: Based on three-dimensional magnetotelluric sounding results

  • Institute of Geophysical and Geochemical Exploration, CAGS, Langfang 065000, Hebei, China

    • Fund Project: Supported by the National Natural Science Foundation of China (No.41574068), the National Key R & D project (2016YFC0600201), China Geological Survey project (No.121201108000160913, No.12120114005801, No.DD20160082, No. DD20190032), and Basic Scientific Research project of CAGS(No.AS2016J12)
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  • Author Bio: QIU Gengen, male, born in 1984, master, senior engineer, mainly engaged in the research and application of magnetotelluric method; E-mail:qiugengen@igge.cn
Received Date:  11 May 2019
Revised Date:  19 July 2019
Publish Date:  25 August 2019
    Abstract

  • South China has experienced the evolution of multiple stages of tectonic-magma-mineralization. It is rich in mineral resources and has multiple mineralization concentration areas, which constitute an important base for national economic development. In this paper, the three-dimensional electrical structure model of the northern part of Wuyi Mountain and adjacent areas is constructed by using the regional magnetotelluric array observation data acquired in south China and the three-dimensional inversion program of WSINV3DMT. The electrical characteristics of the model show that the deep electrical characteristics along the lower part of the fault zone exhibit obvious low resistivity anomalous zones. The low resistivity anomalous zones may be the response of deep and large faults or the assembling boundary of paleo-micro-continental blocks, which have obviously controlled the shallow fault structure. It is found that most of the major endogenous metal deposits in Wuyi area are located above the low resistivity anomaly zone and the edge of deep soft fluids. They have obvious distribution regularity. At the same time, they are mainly distributed in the gradient zone of ΔT polarized magnetic anomaly. Combined with the above distribution rules and characteristics, the favorable areas for prospecting can be preliminarily delineated in Wuyi area.

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