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贵州区域地热成因探讨

王亮, 胡从亮, 张嘉玮, 陈国勇, 张美雪, 杨武, 张应文. 2022. 贵州区域地热成因探讨. 物探与化探, 46(2): 304-315. doi: 10.11720/wtyht.2022.1228
引用本文: 王亮, 胡从亮, 张嘉玮, 陈国勇, 张美雪, 杨武, 张应文. 2022. 贵州区域地热成因探讨. 物探与化探, 46(2): 304-315. doi: 10.11720/wtyht.2022.1228
WANG Liang, HU Cong-Liang, ZHANG Jia-Wei, CHEN Guo-Yong, ZHANG Mei-Xue, YANG Wu, ZHANG Ying-Wen. 2022. Exploration of the genesis of regional geothermal resources in Guizhou Province. Geophysical and Geochemical Exploration, 46(2): 304-315. doi: 10.11720/wtyht.2022.1228
Citation: WANG Liang, HU Cong-Liang, ZHANG Jia-Wei, CHEN Guo-Yong, ZHANG Mei-Xue, YANG Wu, ZHANG Ying-Wen. 2022. Exploration of the genesis of regional geothermal resources in Guizhou Province. Geophysical and Geochemical Exploration, 46(2): 304-315. doi: 10.11720/wtyht.2022.1228

贵州区域地热成因探讨

  • 基金项目:

    贵州省地质矿产勘查开发局重大科研专项“黔西北地区铅锌找矿攻关“(黔地矿纪要(2015)14号)

    贵州省地质物探开发应用工程技术研究中心项目(黔科合[2016]平台人才5401)

    贵州省科技计划项目“贵州省地质调查院院士工作站“(黔科合平台人才[2018]5626)

详细信息
    作者简介: 王亮(1962-),男,研究员,主要从事物探勘查和研究工作。Email: wangliang62@163.com
  • 中图分类号: P314.1;P314.2;P314.3

Exploration of the genesis of regional geothermal resources in Guizhou Province

  • 关于贵州地热成因,人们多倾向于地震活动和断裂控制“地温梯度“机械能升温,不具备岩浆热源及放射性产热条件。本文通过研究前人成果和热储、盖层特征及区域重磁等资料,推测深部断裂和中酸性、基性—超基性岩体,分析天然地热及地热井的区域分布特性,并结合有关的地质资料,提出贵州地热可能存在2种基本成因模式:一是深部断裂控制的“地温梯度“自动增温循环生热,该导热方式驱使地下水持续升温最为发育,二是岩浆岩余热作用,此导热方式的推测作为一种新的产热类型及成因来源补充,而贵州作为我国重要的铀、钍等资源区域成矿地区,目前研究程度低、资料少、规模小,是否存在放射性生热基础尚不清楚。对地热成因深入研究,可为下步区内精准地热调查和找矿方向拓展提供相关依据。
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出版历程
收稿日期:  2021-04-26
刊出日期:  2022-06-28

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