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南岭地区千里山岩体的空间形态及其与成矿的关系

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宋才见, 李谭伟, 叶颖颖, 姚伟, 曾芳. 2020. 南岭地区千里山岩体的空间形态及其与成矿的关系[J]. 中国地质, 47(4): 998-1009. doi: 10.12029/gc20200407
引用本文: 宋才见, 李谭伟, 叶颖颖, 姚伟, 曾芳. 2020. 南岭地区千里山岩体的空间形态及其与成矿的关系[J]. 中国地质, 47(4): 998-1009. doi: 10.12029/gc20200407
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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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南岭地区千里山岩体的空间形态及其与成矿的关系

  • 湖南省地球物理地球化学勘查院, 湖南 长沙 410116

  • 基金项目:
    中国地质调查局“湖南千里山—瑶岗仙地区1：5万区域地质综合调查”子项目（12120114033401）资助
详细信息
    作者简介: 宋才见, 男, 1962年生, 研究员级高级工程师, 主要从事地球物理勘查综合研究; E-mail:scj-wt@163.com

  • 中图分类号: P588.12+1

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)
More Information
    Author Bio: SONG Caijian, male, born in 1962, senior engineer, mainly engages in comprehensive geophysical exploration research; E-mail:scj-wt@163.com .

    摘要

  • 千里山岩体是南岭地区与锡钨等矿产成矿关系密切的重要岩体，研究其空间特征与控矿作用，对于深部地质填图以及深部找矿预测具有重要意义。利用中比例尺重力资料，确定了千里山岩体的隐伏边界；通过对千里山岩体进行二维、三维模拟反演，揭示了千里山岩体与王仙岭岩体的连接关系和空间形态特征以及与围岩的接触关系。推断认为：千里山岩体与王仙岭岩体在深部相连，呈大岩基产出，并受到深大断裂控制；两岩体三维形态整体表现为气球膨胀式轮廓。结合地质资料，探讨了千里山岩体与成矿的关系，分析认为深部岩基和构造为矿床提供了成矿物质来源、热源及上升通道。

    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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  • 图 1  千里山—瑶岗仙地区区域构造格架

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  千里山地区地质矿产图

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  千里山—王仙岭半隐伏岩体推断成果

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  千里山半隐伏岩体剖面重力反演推断成果

    Figure 4. 

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    图 5  千里山岩体三维空间分布形态

    Figure 5. 

    下载: 全尺寸图片 幻灯片

    图 6  千里山—王仙岭半隐伏岩体与矿产分布关系

    Figure 6. 

    下载: 全尺寸图片 幻灯片

    表 1  千里山地区主要地层及岩体密度值一览

    Table 1.  A survey of the main strata and rock mass density values in the Qianli Mountain

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修回日期:  2020-02-28
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