甘肃临泽县城区深部地热资源调查评价

doi:10.11720/wtyht.2020.0191

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摘要

临泽县位于张掖—民乐盆地西南缘,祁连山褶皱带中北部,具有较好的开发利用地热资源的前景。本文通过分析研究区区域地质构造、水文地质特征等,在已有地热井旁和重点工作区开展广域电磁法测深工作,以区域水文地质为基础,以物探勘查成果为依据,解释推断了研究区地质构造及岩体的分布特征,分析评价了研究区地热勘查前景,同时,初步构建了研究区地热勘查“地质—地球物理—地热”模型,为研究区及邻区的地热勘查提供借鉴和指导。

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	李麒麟
	李荣亮
	苏海伦
	刘洋
	曹自才

关键词 ：水文地质, 地热资源, 广域电磁法, 地质构造, 甘肃

Abstract：

Linze County is located at the southwest edge of Zhangye-Minle basin and along northern central Qilian fold belt and has a good prospect for development and utilization of geothermal resources. The authors analyzed regional geological structure and hydrogeological characteristics of the study area and investigated existing geothermal well and preferred working area by the wide field electromagnetic method. Through comprehensive analysis and on the basis of regional hydrogeologic and geophysical exploration results, the distribution characteristics of geological structure and rock mass in the study area were interpreted and inferred, the prospect of geothermal exploration in the research area was analyzed and evaluated. Meanwhile,the "geology-geophysical-geothermal energy" model of geothermal exploration in the study area was preliminarily constructed. This model provides reference and guidance for geothermal exploration in the study area and adjacent areas.

Key words： hydrogeology geothermal resources wide field electromagnetic method geological structure Gansu Province

收稿日期: 2020-04-21 出版日期: 2020-10-26

:	P641.7
	P631

通讯作者: 李荣亮

作者简介: 李麒麟(1970-),男,高级工程师,长期从事水工环项目生产、管理、研究工作。

引用本文:

李麒麟, 李荣亮, 苏海伦, 刘洋, 曹自才. 甘肃临泽县城区深部地热资源调查评价[J]. 物探与化探, 2020, 44(5): 999-1008.
LI Qi-Lin, LI Rong-Liang, SU Hai-Lun, LIU Yang, CAO Zi-Cai. Investigation evaluation and method study of deep geothermal resources in Linze County, Gansu Province. Geophysical and Geochemical Exploration, 2020, 44(5): 999-1008.

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https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2020.0191 或 https://www.wutanyuhuatan.com/CN/Y2020/V44/I5/999

Fig.1 研究区大地构造简图

Fig.2 研究区地下水补给模式

Table 1 研究区地层电性特征

Fig.3 研究区地热资源调查物探工作布置及综合成果平面示意

Fig.4 L0线(a)和L1线(b)电阻率一维连续介质反演断面及解释推断

Fig.5 孔隙型含水层测井曲线特征

Fig.6 裂隙型含水层测井曲线特征

Table 2 已有地热井地层结构

Fig.7 L2线电阻率一维连续介质反演断面及解释推断

Fig.8 L6线电阻率一维连续介质反演断面及解释推断

Fig.9 L2线地质综合解释

Fig.10 L6线地质综合解释

Fig.11 研究区“地质—地球物理—地热”模型构建

[1]	中国石油地质志编委会. 中国石油地质志玉门卷[M]. 北京: 石油工业出版社, 1989.
[1]	China Petroleum Geology Editorial Board. China petroleum geology journal Yumen volume [M]. Beijing: Petroleum Industry Press, 1989.
[2]	刘兴春. 民乐山前平原新构造运动及其对地下水埋藏的影响[J]. 甘肃地质学报, 2000,9(1):74-79.
[2]	Liu X C. Neo-tectonic movement of the Minle Piedmont Plain and its impact on groundwater burial[J]. Acta Geologica Gansu, 2000,9(1):74-79.
[3]	赵聚林, 刘多朝. 概论祁连山前民乐盆地隐伏构造、第四系及地下水——依据1:10万综合电法成果[J]. 甘肃地质学报, 2005,14(1):82-85.
[3]	Zhao J L, Liu D C. The hidden faults and quaternary system of Minle basin in front of the Qilian mountain[J]. Acta Geologica Gansu, 2005,14(1):82-85.
[4]	俞兆虎, 滕汉仁, 李百祥. 张掖—民乐盆地地质—地球物理信息揭示的地热资源前景与勘查方法优化组合[J]. 甘肃地质, 2018,27(s1):79-84.
[4]	Yu Z H, Teng H R, Li B X. On geothermal resource potential and optimization prospecting methods in terms of geology-geophysical information in Zhangye-Minle basin[J]. Gansu Geology, 2018,27(s1):79-84.
[5]	张振杰, 李兴海, 胡潇. 综合物探方法在张掖城区及外围深部地热资源勘查中的应用研究[J]. 地下水, 2018,40(4):52-54.
[5]	Zhang Z J, Li X H, Hu X. Application of comprehensive geophysical methods in the exploration of deep geothermal resources in Zhangye city and its periphery[J] . Groundwater, 2018,40(4):52-54.
[6]	何继善. 广域电磁法和伪随机信号电法[M]. 北京: 高等教育出版社, 2010.
[6]	He J S. Wide area electromagnetic method and pseudo-random signal electrical method[M]. Beijing: Higher Education Press, 2010.
[7]	何继善. 广域电磁测深法研究[J]. 中南大学学报:自然科学版, 2010,41(3):1065-1072.
[7]	He J S. Wide field electromagnetic sounding methods[J]. Journal of Central South University:Science and Technology, 2010,41(3):1065-1072.
[8]	李帝铨, 胡艳芳. 强干扰矿区中广域电磁法与CSAMT探测效果对比[J]. 物探与化探, 2015,39(5):967-972. doi: 10.11720/wtyht.2015.5.15
[8]	Li D Q, Hu Y F. A comparison of wide field electromagnetic method with CSAMT method in strong interferential mining area[J]. Geophysical and Geochemical Exploration, 2015,39(5):967-972. doi: 10.11720/wtyht.2015.5.15
[9]	朱裕振, 许聪悦. 广域电磁法深部找矿实验效果[J]. 物探与化探, 2011,35(6):743-746.
[9]	Zhu Y Z, Xu C Y. The experimental application of wider field electromagnetic method to the prospectiang for deep ore deposits[J]. Geophysical and Geochemical Exploration, 2011,35(6):743-746.
[10]	凌帆, 朱裕振, 周明磊, 等. 广域电磁法在南华北盆地长山隆起页岩气资源潜力评价中的应用[J]. 物探与化探, 2017,41(2):369-376.
[10]	Ling F, Zhu Y Z, Zhou M L, et al. Shale gas potential assessment of Changsan uplift area in southern North China basin by using wide field electromagnetic method[J]. Geophysical and Geochemical Exploration, 2017,41(2):369-376.
[11]	曹彦荣, 宋涛, 韩红庆, 等. 用广域电磁法勘查深层地热资源[J]. 物探与化探, 2017,41(4):678-683.
[11]	Cao Y R, Song T, Han H Q, et al. Exploration of deep geothermal energy resources with wide field electromagnetic method[J]. Geophysical and Geochemical Exploration, 2017,41(4):678-683.
[12]	孙求实, 袁杰, 宗文明, 等. 广域电磁法在辽西地区牛营子凹陷油气资源潜力评价中的应用[J]. 物探与化探, 2019,34(1):64-69.
[12]	Sun Q S, Yuan J, Zong W M, et al. The application of wide field electromagnetic method to the oil and gas exploration of Niuyingzi sag in Liaoxi area[J]. Geophysical and Geochemical Exploration, 2019,43(1):64-69.
[13]	郑文俊. 河西走廊及其邻区活动构造图像及构造变形模式[D]. 北京:中国地震局地质研究所, 2009.
[13]	Zheng W J. Active tectonic image and tectonic deformation model of Hexi Corridor and its adjacent area [D]. Beijing: Institute of Geology, China Earthquake Administration, 2009.
[14]	陈文彬. 河西走廊及邻近地区最新构造变形基本特征及构造成因分析[D]. 北京:中国地震局地质研究所, 2003.
[14]	Chen W B. Analysis of the latest tectonic characteristics and tectonic genesis of the Hexi Corridor and its adjacent areas[D]. Beijing: Institute of Geology, China Earthquake Administration, 2003.
[15]	魏红军, 李百祥. 张掖—民乐盆地地质构造特征与张掖市地热资源开发可行性分析[J]. 甘肃地质, 2007(4):73-76,84.
[15]	Wei H J, Li B X. Characteristics of geological structures in Zhangye-Minle basin and feasibility study of Geothermal resources in Zhangye city[J]. Gansu Geology, 2007(4):73-76,84.
[16]	谭美娟. 河西走廊榆木山东麓第四纪地层研究[D]. 北京: 中国地质大学(北京), 2016.
[16]	Tan M J. Quaternary stratigraphy of the eastern foot of Elm in the Hexi Corridor[D]. Beijing: China University of Geosciences (Beijing), 2016.
[17]	丁宏伟, 张举. 河西走廊深层地下水的赋存和开发[J]. 西北地质, 2009,42(3):109-119.
[17]	Ding H W, Zhang J. Occurrence and development of deep underground water in Hexi Corridor[J]. Northwestern Geology, 2009,42(3):109-119.
[18]	张光辉, 刘少玉, 张翠云, 等. 黑河流域地下水循环演化规律研究[J]. 中国地质, 2004,31(3):289-293.
[18]	Zhang G H, Liu S Y, Zhang C Y, et al. Evolution of groundwater circulation in the Heihe river drainage area[J]. Geology in China, 2004,31(3):289-293.

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