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东南沿海干热岩资源成因模式探讨及勘查进展

李亭昕 蔺文静 甘浩男 岳高凡 张德龙 王贵玲

李亭昕, 蔺文静, 甘浩男, 等, 2020. 东南沿海干热岩资源成因模式探讨及勘查进展. 地质力学学报, 26 (2): 187-200. DOI: 10.12090/j.issn.1006-6616.2020.26.02.018
引用本文: 李亭昕, 蔺文静, 甘浩男, 等, 2020. 东南沿海干热岩资源成因模式探讨及勘查进展. 地质力学学报, 26 (2): 187-200. DOI: 10.12090/j.issn.1006-6616.2020.26.02.018
LI Tingxin, LIN Wenjing, GAN Haonan, et al., 2020. Research on the genetic model and exploration progress of hot dry rock resources on the southeast coast of China. Journal of Geomechanics, 26 (2): 187-200. DOI: 10.12090/j.issn.1006-6616.2020.26.02.018
Citation: LI Tingxin, LIN Wenjing, GAN Haonan, et al., 2020. Research on the genetic model and exploration progress of hot dry rock resources on the southeast coast of China. Journal of Geomechanics, 26 (2): 187-200. DOI: 10.12090/j.issn.1006-6616.2020.26.02.018

东南沿海干热岩资源成因模式探讨及勘查进展

doi: 10.12090/j.issn.1006-6616.2020.26.02.018
基金项目: 

国家自然科学基金应急管理项目 41741018

国家重点研发计划课题 2018YFA0404104

中国地质调查局二级项目 DD20160191

详细信息
    作者简介:

    李亭昕(1992-), 女, 在读硕士, 主要从事地热、地球化学相关研究。E-mail:litingxin0324@qq.com

    通讯作者:

    蔺文静(1978-), 男, 博士, 主要从事地热、干热岩勘查开发相关研究工作。E-mail:lwenjing@msn.com

  • 中图分类号: P314

Research on the genetic model and exploration progress of hot dry rock resources on the southeast coast of China

  • 摘要: 干热岩是一种重要的地热资源,绝大部分以开采地壳中生代以来中酸性侵入岩体中所蕴含的热量为主。东南沿海地区是中国最主要的高放射性花岗岩分布区,发育大面积的中生代酸性花岗岩体,是寻找干热岩的良好靶区。通过研究东南沿海大地构造背景、区域大地热流分布、地壳厚度、居里面埋深及新构造等条件,分析了东南沿海干热岩资源的赋存背景,对福建地区是否存在干热岩进行了探讨,并通过控热构造分析提出了东南沿海干热岩资源的成因模式,初步建立了东南沿海干热岩成藏的三元聚热模型,总结了漳州、惠州等地区的干热岩资源靶区勘查进展,相关研究为今后中国东南沿海地区干热岩勘查评价提供了基础。

     

  • 图  1  东南沿海部分地区地壳厚度图(Guo et al., 2019)

    Figure  1.  Crust thickness of the southeast coast of China(Guo et al., 2019)

    图  2  YCA测线P波波速等值线剖面图(熊绍柏等,1991)

    Figure  2.  Contour profile of the P-wave velocity of the survey line YCA(Xiong et al., 1991)

    图  3  江西南部—福建—台湾综合地球物理剖面图(Zhou and Li, 2000)

    Figure  3.  Integrated geophysical profiles of southern Jiangxi-Fujian-Taiwan(Zhou and Li, 2000)

    图  4  中国东南沿海地区大地热流值等值线图(蔺文静等,2016)

    Figure  4.  Contour map of terrestrial heat flow values on the southeast coast of China(Lin et al., 2016)

    图  5  东南沿海干热岩资源成藏的三元聚热模式图

    Figure  5.  Three-way heat accumulation model for dry hot rock resources on the southeast coast of China

    图  6  漳州地区地质简图(A-A′为物探综合剖面)(蔺文静等,2015)

    Figure  6.  Geological map of Zhangzhou area, A-A′ as the geophysical prospecting composite profile (Lin et al., 2015)

    图  7  龙海地区重力和大地电磁联合反演推断解释剖面A-A′(剖面位置见图 6)(蔺文静等,2019)

    Figure  7.  Joint inversion interpretation of gravity and magnetotelluric of profile A-A′ in Longhai area, profile shown in Fig 6.(Lin et al., 2019)

    图  8  漳州龙海地区4000 m井深测井温度曲线

    Figure  8.  4000 m logging temperature curves in Longhai area, Zhangzhou

    图  9  研究区深部地温分布图

    Figure  9.  Deep geothermal map of the study area

    图  10  黄沙洞地区地质简图及物探解译成果图

    Figure  10.  Geological map and geophysical prospecting interpretation map in Huangshadong area

    图  11  L2和L4测线联合解译图

    Figure  11.  Joint interpretation profile of survey line L2 and L4

    图  12  L1和L3测线联合解译图

    Figure  12.  Joint interpretation profile of survey line L1 and L3

    图  13  惠州惠热1井地温测温曲线

    Figure  13.  Geothermal temperature curve of Huire Well 1 in Huizhou

    表  1  东南沿海地区不同岩石类型的单位体积生热率(赵平等,1995林乐夫等,2017)

    Table  1.   Heat production per unit volume of different rock types on the southeast coast of China(Zhao et al., 1995; Lin et al., 2017)

    岩石类型平均单位体积生热率/
    (μW/m3)
    不同时代花岗岩晋宁期花岗岩3.1
    加里东期花岗岩3.3
    印支期花岗岩3.9
    燕山早期花岗岩5.2
    燕山晚期花岗岩6.4
    凝灰岩2.7
    碳酸盐岩0.59
    下载: 导出CSV

    表  2  模型主要参数表

    Table  2.   Main parameters of the model

    模型部分孔隙度渗透率/
    m2
    热导率/
    W/(m·K)
    热储0.011×10-173.4
    浅部断裂0.051×10-125.5
    深部断裂0.021×10-175.5
    下载: 导出CSV
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出版历程
  • 收稿日期:  2019-11-03
  • 修回日期:  2020-01-10
  • 刊出日期:  2020-04-28

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