山东省聊城市东部地热田地热资源特征
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摘要
山东省聊城东部地热田内蕴藏着丰富的地热资源,地质构造条件、热储地质条件都比较有利,是开发地热资源的有利地段。通过对已有钻探资料的分析,结合近年来的勘查项目研究成果,笔者认为聊城东部地热田属于岩溶裂隙层状传导型地热田,区域地质构造主要为聊考断裂和茌平断裂,热储层主要为奥陶纪马家沟组灰岩地层,该区的地温梯度主要受构造控制,断裂导热是形成本区地热田的一个重要因素,地下热水矿化度较小,含有多种对人体有益的矿物、元素,并且根据开发现状提出了合理的开发利用与保护政策。
Geothermal resources are very rich in the geothermal field of eastern Liaocheng,Shandong Province. Geological-structural conditions and geothermal reservoirs there are relatively favorable for the exploitation of these resources.Based on drilling data and recent research results,the author considers that the Liaocheng geothermal field belongs to the karst fissure layered conductive type,with the regional geological structures being mainly composed of Liaokao fault and Chiping fault,and the hot reservoir chiefly comprised of limestone strata of Ordovician Majiagou Formation.The geothermal gradient of the area is controlled mainly by structure,the structural heat conduction is a key factor for the formation of this area,the mineralization intensity of the geothermal water is low,and the geothermal water contains some useful mineral components.Some suggestions concerning the reasonable development of geothermal resources and some policies for solving problems in current exploitation work are also put forward in this paper.
Geothermal resources are very rich in the geothermal field of eastern Liaocheng,Shandong Province. Geological-structural conditions and geothermal reservoirs there are relatively favorable for the exploitation of these resources.Based on drilling data and recent research results,the author considers that the Liaocheng geothermal field belongs to the karst fissure layered conductive type,with the regional geological structures being mainly composed of Liaokao fault and Chiping fault,and the hot reservoir chiefly comprised of limestone strata of Ordovician Majiagou Formation.The geothermal gradient of the area is controlled mainly by structure,the structural heat conduction is a key factor for the formation of this area,the mineralization intensity of the geothermal water is low,and the geothermal water contains some useful mineral components.Some suggestions concerning the reasonable development of geothermal resources and some policies for solving problems in current exploitation work are also put forward in this paper.
引文
[1]山东省地质科学实验研究院.山东省聊城市单官屯地热单井地质报告,2006.
[1]山东省地质科学研究所.山东省前晚第三纪基岩地质图(1:50万)及说明书,1982.
[1]山东省地质环境监测总站.京九沿线(山东段)地质矿产资源开发与经济发展研究,1999.
[1]方保明.山东省地热资源综合信息远景预测[D].长春:吉林大学, 2006. Fang Baoming.Perspective Prognosis on Geothermal Resource in Synthetic Information in Shandong Province[D].Changchun:Jilin University,2006(in Chinese with English abstract).
[2]徐军祥,康凤新.山东省地热资源[J].中国地质,2000,10(2):41-42. Xu Junxiang,Kang Fengxin.Geological resources in Shandong Province[J].Geology in China,2000,10(2):41-42(in Chinese with English abstract).
[3]王奎峰.聊城西部地热田地热资源赋存特征研究[J].地质灾害与环境保护,2008,19(1):52-56. Wang Kuifeng.Bearing features of geothermal resources in geothermal field in west part of Liaocheng[J].Journal of Geological Hazards and Environment Preservation,2008,19(1):52-56(in Chinese with English abstract).
[4]李坷凌,宋丽红.濮阳市地热资源特征[J].水文地质工程地质, 2004,31(6):78-81. Li Keling,Song Lihong.Characteristics of the geothermal resources in Puyang[J].Hydrogeology & Engineering Geology,2004,31(6): 78-81(in Chinese with English abstract).
[5]王奎峰,母国妍,赵群.临清市区地热资源特征及开发探讨[J].地质调查与研究,2007,30(3):224-229. Wang Kuifeng,Mu Guoyan,Zhao Qun.A tentative discussion on the geothermal resources characteristics and exploitation in Linqing city[J].Geological Survey and Research,2007,30(3):224-229(in Chinese with English abstract).
[6]郭德科,赵卫红,李炳文.冀鲁豫交界区地下流体模糊熵值的变化与地震的关系[J].地震研究,2003,26(1):80-83. Guo Deke,Zhao Weihong,Li Bingwen.Relations between the earthquake and the fussy entropy variation for subsurface fluid in the joint area of Hebei,Shandong and Henan Province[J].Journal of Seismological Research,2003,26(1):80-83(in Chinese with English abstract).
[7]李秀英,蔡洪涛,任清岭.沧州市区地热地质特征及地热资源开发探讨[J].地球学报,2000,21(2):171-176. Li Xiuying,Cai Hongtao,Ren Qingling.A tentative discussion on the geothermo-geological characteristics and development of geothermal resources in Cangzhou city[J].Acta Geoscientia Sinica, 2000,21(2):171-176(in Chinese with English abstract).
[8]石维栋,张森琦,周金元,等.西宁盆地北西缘地下热水分布特征[J].中国地质,2006,33(5):1131-1136. Shi Weidong,Zhang Senqi,Zhou Jinyuan,et al.Distribution characteristics of geothermal water on the northwestern margin of the Xining basin[J].Geology in China,2006,33(5):1131-1136(in Chinese with English abstract).
[9]王佟,王莹.陕西渭河盆地地热资源赋存特征研究[J].西安科技学院学报,2004,24(1):83-85. Wang Tong,Wang Ying.Bearing features of geothermal resources in Weihe basin of Shaanxi[J].Jounal of Xi'an University of Science and Techonlogy,2004,24(1):83-85(in Chinese with English abstract).
[10]杨庆锦,王招香.YW-Ⅲ型岩性测深仪在聊城地热勘查的效果[J].地质与勘探,2004,40(Z1):49-52. Yang Qingjin,Wang Zhaoxiang.Effects of geothermal prospecting with YW-Ⅲelectrotelluric field lithological sounding at the Liaocheng area[J].Geology and Prospecting,2004,40(Z1):49-52 (in Chinese with English abstract).
[11]陈墨香.华北地热[M].北京:科学出版社,1988:50-52. Chen Moxiang.Huabei Geothermal[M].Beijing:Science Press, 1988:50-52(in Chinese with English abstract).
[12]陈静生.水环境化学[M].北京:高等教育出版社,1991:20-24. Chen Jingsheng.Aquatic Environmental Chemistry[M].Beijing: High Education Press,1991:20-24(in Chinese with English abstract).
[13]颜世强,潘懋,邹祖光,等.山东德州凹陷地下热水地球化学特征及成因[J].中国地质,2007,34(1):150-151. Yan Shiqiang,Pan Mao,Zou Zuguang,et al.Geochemical characteristics and origin of geothermal water in the Dezhou hollow[J].Geology in China,2007,34(1):149-152(in Chinese with English abstract).
[14]沈照理,朱宛华,等.水文地球化学基础[M].北京:地质出版社, 1999,87-88. Shen Zhaoli,Zhu Wanhua,et al.Introduction to Hydrogeochemistry [M].Beijing:Geological Publishing House,1999:87-88(in Chinese with English abstract).
[15]郑永飞,陈江峰.稳定同位素地球化学[M].北京:科学出版社, 2000,152-153. ??Zhen Yongfei,Chen Jiangfeng.Stable Isotope Geochemistry[M]. Beijing:Science Press,2000:152-153(in Chinese with English abstract).
[16]王宝玉.河南省地热资源开发利用现状及展望[J].地质与勘探, ??1999,35(1):47-48. Wang Baoyu.Development of geothermal resources in Henan[J]. Geology and Prospecting,1999,35(1):47-48(in Chinese with English abstract).
[1]山东省地质科学研究所.山东省前晚第三纪基岩地质图(1:50万)及说明书,1982.
[1]山东省地质环境监测总站.京九沿线(山东段)地质矿产资源开发与经济发展研究,1999.
[1]方保明.山东省地热资源综合信息远景预测[D].长春:吉林大学, 2006. Fang Baoming.Perspective Prognosis on Geothermal Resource in Synthetic Information in Shandong Province[D].Changchun:Jilin University,2006(in Chinese with English abstract).
[2]徐军祥,康凤新.山东省地热资源[J].中国地质,2000,10(2):41-42. Xu Junxiang,Kang Fengxin.Geological resources in Shandong Province[J].Geology in China,2000,10(2):41-42(in Chinese with English abstract).
[3]王奎峰.聊城西部地热田地热资源赋存特征研究[J].地质灾害与环境保护,2008,19(1):52-56. Wang Kuifeng.Bearing features of geothermal resources in geothermal field in west part of Liaocheng[J].Journal of Geological Hazards and Environment Preservation,2008,19(1):52-56(in Chinese with English abstract).
[4]李坷凌,宋丽红.濮阳市地热资源特征[J].水文地质工程地质, 2004,31(6):78-81. Li Keling,Song Lihong.Characteristics of the geothermal resources in Puyang[J].Hydrogeology & Engineering Geology,2004,31(6): 78-81(in Chinese with English abstract).
[5]王奎峰,母国妍,赵群.临清市区地热资源特征及开发探讨[J].地质调查与研究,2007,30(3):224-229. Wang Kuifeng,Mu Guoyan,Zhao Qun.A tentative discussion on the geothermal resources characteristics and exploitation in Linqing city[J].Geological Survey and Research,2007,30(3):224-229(in Chinese with English abstract).
[6]郭德科,赵卫红,李炳文.冀鲁豫交界区地下流体模糊熵值的变化与地震的关系[J].地震研究,2003,26(1):80-83. Guo Deke,Zhao Weihong,Li Bingwen.Relations between the earthquake and the fussy entropy variation for subsurface fluid in the joint area of Hebei,Shandong and Henan Province[J].Journal of Seismological Research,2003,26(1):80-83(in Chinese with English abstract).
[7]李秀英,蔡洪涛,任清岭.沧州市区地热地质特征及地热资源开发探讨[J].地球学报,2000,21(2):171-176. Li Xiuying,Cai Hongtao,Ren Qingling.A tentative discussion on the geothermo-geological characteristics and development of geothermal resources in Cangzhou city[J].Acta Geoscientia Sinica, 2000,21(2):171-176(in Chinese with English abstract).
[8]石维栋,张森琦,周金元,等.西宁盆地北西缘地下热水分布特征[J].中国地质,2006,33(5):1131-1136. Shi Weidong,Zhang Senqi,Zhou Jinyuan,et al.Distribution characteristics of geothermal water on the northwestern margin of the Xining basin[J].Geology in China,2006,33(5):1131-1136(in Chinese with English abstract).
[9]王佟,王莹.陕西渭河盆地地热资源赋存特征研究[J].西安科技学院学报,2004,24(1):83-85. Wang Tong,Wang Ying.Bearing features of geothermal resources in Weihe basin of Shaanxi[J].Jounal of Xi'an University of Science and Techonlogy,2004,24(1):83-85(in Chinese with English abstract).
[10]杨庆锦,王招香.YW-Ⅲ型岩性测深仪在聊城地热勘查的效果[J].地质与勘探,2004,40(Z1):49-52. Yang Qingjin,Wang Zhaoxiang.Effects of geothermal prospecting with YW-Ⅲelectrotelluric field lithological sounding at the Liaocheng area[J].Geology and Prospecting,2004,40(Z1):49-52 (in Chinese with English abstract).
[11]陈墨香.华北地热[M].北京:科学出版社,1988:50-52. Chen Moxiang.Huabei Geothermal[M].Beijing:Science Press, 1988:50-52(in Chinese with English abstract).
[12]陈静生.水环境化学[M].北京:高等教育出版社,1991:20-24. Chen Jingsheng.Aquatic Environmental Chemistry[M].Beijing: High Education Press,1991:20-24(in Chinese with English abstract).
[13]颜世强,潘懋,邹祖光,等.山东德州凹陷地下热水地球化学特征及成因[J].中国地质,2007,34(1):150-151. Yan Shiqiang,Pan Mao,Zou Zuguang,et al.Geochemical characteristics and origin of geothermal water in the Dezhou hollow[J].Geology in China,2007,34(1):149-152(in Chinese with English abstract).
[14]沈照理,朱宛华,等.水文地球化学基础[M].北京:地质出版社, 1999,87-88. Shen Zhaoli,Zhu Wanhua,et al.Introduction to Hydrogeochemistry [M].Beijing:Geological Publishing House,1999:87-88(in Chinese with English abstract).
[15]郑永飞,陈江峰.稳定同位素地球化学[M].北京:科学出版社, 2000,152-153. ??Zhen Yongfei,Chen Jiangfeng.Stable Isotope Geochemistry[M]. Beijing:Science Press,2000:152-153(in Chinese with English abstract).
[16]王宝玉.河南省地热资源开发利用现状及展望[J].地质与勘探, ??1999,35(1):47-48. Wang Baoyu.Development of geothermal resources in Henan[J]. Geology and Prospecting,1999,35(1):47-48(in Chinese with English abstract).
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