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SONG Caijian, LI Tanwei, YE Yingying, YAO Wei, ZENG Fang. 2020. Spatial morphology of Qianlishan rock mass and its relationship with mineralization in Nanling region[J]. Geology in China, 47(4): 998-1009. doi: 10.12029/gc20200407
Citation: SONG Caijian, LI Tanwei, YE Yingying, YAO Wei, ZENG Fang. 2020. Spatial morphology of Qianlishan rock mass and its relationship with mineralization in Nanling region[J]. Geology in China, 47(4): 998-1009. doi: 10.12029/gc20200407
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Spatial morphology of Qianlishan rock mass and its relationship with mineralization in Nanling region

  • Hunan Academy of Geophysical and Geochemical Exploration, Changsha 410116, Hunan, China

    • Fund Project: Supported by the project of China Geological Survey (No. 12120114033401)
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  • Author Bio: SONG Caijian, male, born in 1962, senior engineer, mainly engages in comprehensive geophysical exploration research; E-mail:scj-wt@163.com
Received Date:  29 March 2019
Revised Date:  28 February 2020
Publish Date:  25 August 2020
    Abstract

  • Qianlishan rock mass is an important rock mass closely related to tin and tungsten mineralization in Nanling region. Studying its spatial characteristics and ore-controlling role is of great significance for deep geological mapping and deep prospecting and prediction. Using medium-scale gravity data the authors determined the hidden boundary of Qianlishan rock mass. Two-dimensional and three-dimensional simulation inversion revealed the connection relationship between Qianlishan rock mass and Wangxianling rock mass, the spatial morphological characteristics and the contact relationship with surrounding rock masses. It is inferred that the Qianlishan rock mass and the Wangxianling rock mass are connected in depth, and were produced in a large basement and controlled by deep and large faults, with the three-dimensional shape of the two rock masses being balloon expansive contour as a whole. On the basis of geological data, the relationship between Qianlishan rock mass and mineralization was discussed. It is concluded that deep bedrock and structure provided ore-forming material source, heat source and ascending channel for the deposit.

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