河南省上蔡县地热系统成因模式及开发潜力

赵雅静 ,  孙福利 ,  冷济高 ,  潘良云 ,  曹海丽 ,  高阳

东北石油大学学报 ›› 2025, Vol. 49 ›› Issue (5) : 12 -23.

PDF (20963KB)
东北石油大学学报 ›› 2025, Vol. 49 ›› Issue (5) : 12 -23. DOI: 10.3969/j.issn.2095-4107.2025.05.002
油气地质与勘探

河南省上蔡县地热系统成因模式及开发潜力

作者信息 +

Geological genesis and development potential of geothermal system in Shangcai County, Henan Province

Author information +
文章历史 +
PDF (21465K)

摘要

河南省上蔡县地热系统是典型的水热型地热系统。根据地质调查、地震、钻测井资料及地球化学数据,研究上蔡县地热系统地热地质特征,建立地热系统成因模式,评价地热资源开发潜力,明确地热勘探开发有利区。结果表明:上蔡县地热系统是典型的中-低温传导型地热系统,局部断裂发育,大地热流和地温梯度高于区域背景;发育新近系、古近系和寒武系一奥陶系三套热储层,第四系厚层泥岩为区域性盖层;地热水来源为遂平一带低山丘陵地区的大气降水,沿不整合面人渗,在循环过程中,经深部地幔热传导增温在热储层中富集;热储层总静态资源量约为 3.77×1013 kJ ,水量为 6.42×108 m3 ,折合标准煤为 1.29×106t ,可满足 6.71×105 m2 的供暖面积需求,上蔡县城区为勘探开发有利区。该结果为河南省上蔡县及邻区的地热资源开发提供指导。

Abstract

Shangcai County, Henan Province is a typical hydrothermal system in the sedimentary basin. Based on comprehensive geological surveys, seismic, drilling, logging data and geochemical data, a comprehensive study of the geothermal geological characteristics of the geothermal system in Shangcai County will be conducted. The geothermal geological elements were systematically analyzed, and the geothermal geological characteristics, genetic geological models, and resource potential were basically clarified. It is considered that Shangcai County is a typical medium-low temperature conductive geothermal system with developed faults and high geothermal background; There are developing three sets of thermal reservoirs in the Neogene, Paleogene, and Cambrian Ordovician systems with thick mudstone layers in the Quaternary system serving as regional cap rocks; This system recharge water source comes from the atmospheric precipitation in the low mountain and hilly areas of Suiping, and its migration channels are un-conformity surface. During the circulation process, the water gradually enriched in the thermal reservoir; According to the fine evaluation results of geothermal resources in Shangcai Area, the total geothermal reserves amount to 3.77×1013 kJ, with a water volume of 6.42×108 m3, equivalent to 1.29×106t of standard coal, and the annual exploitation of geothermal resources can meet the indoor heating area of 6.71×105 million square meters. Comprehensive analysis shows that the urban area of Shangcai County is a favorable area for exploration and development. The study is of theoretical guiding significance for the development of geothermal resources in Shangcai County and its neighboring area.

关键词

地热系统 / 成因模式 / 开发潜力 / 资源量评价 / 上蔡县

Key words

geothermal system / genetic model / develop potential / resources evaluation / Shangcai County

引用本文

引用格式 ▾
赵雅静,孙福利,冷济高,潘良云,曹海丽,高阳. 河南省上蔡县地热系统成因模式及开发潜力[J]. 东北石油大学学报, 2025, 49(5): 12-23 DOI:10.3969/j.issn.2095-4107.2025.05.002

登录浏览全文

4963

注册一个新账户 忘记密码

参考文献

[1]

王贵玲, 陆川. 碳中和目标驱动下地热资源开采利用技术进展[J]. 地质与资源, 2022, 31(3):412-425.

[2]

WANG Guiling, LU Chuan. Progress of geothermal resources exploitation and utilization technology driven by carbon neutralization target[J]. Geology and Resources, 2022, 31(3):412-425.

[3]

庞忠和, 黄少鹏, 胡圣标, . 中国地热研究的进展与展望(1995-2014)[J]. 地质科学, 2014, 49(3):719-727.

[4]

PANG Zhonghe, HUANG Shaopeng, HU Shengbiao, et al. Geothermal studies in China:progress and prospects(1995-2014)[J]. Chinese Journal of Geology, 2014, 49(3):719-727.

[5]

刘德民, 张昌生, 陆婉玲, . 汾渭地堑中、深层地热资源富集背景与形成机制[J]. 地学前缘, 2025, 32(1):367-379.

[6]

LIU Demin, ZHANG Changsheng, LU Wanling, et al. Enrichment background and formation mechanism of middle and deep geothermal resources in Fenwei Graben[J]. Earth Science Frontiers, 2025, 32(1):367-379.

[7]

汪新伟, 王婷濒, 张瑄, . 太原盆地西温庄地热田的成因机制[J]. 地球科学, 2019, 44(3):1042-1056.

[8]

WANG Xinwei, WANG Tinghao, ZHANG Xuan, et al. Genetic mechanism of Xiwenzhuang geothermal field in Taiyuan Basin[J]. Chinese Journal of Geology, 2019, 44(3):1042-1056.

[9]

RYBACH L, MUFFLERL J P. 地热系统:原理和典型地热系统分析[M].佟伟,译. 北京: 地质出版社,1981:1-6.

[10]

RYBACH L, MUFFLERL J P. Geothermal systems:Principles and case histories[M]. TONG Wei,trans.Beijing: Geology Press, 1981:1-6.

[11]

刘常源, 赵增新, 亢品, . 砂岩热储层回灌条件对储层孔渗物性的影响[J/OL]. 特种油气藏,1-13[2025-01-02]. http://kns.cnki.net/ kcms/detail/21.1357.TE.20241127.1352.002.html.

[12]

LIU Changyuan, ZHAO Zengxin, KANG Pin, et al. The influence of reinjection conditions on reservoir porosity and permeability properties in sandstone thermal reservoirs[J/OL]. Special Oil & Gas Reservoirs,1-13[2025-01-02]. http://kns.cnki.net/kcms/detail/21.1357.TE.20241127.1352.002.html.

[13]

何治亮, 冯建吝, 张英, . 试论中国地热单元分级分类评价体系[J]. 地学前缘, 2017, 24(3):168-179.

[14]

HE Zhiliang, FENG Jianyun, ZHANG Ying, et al. A tentative discussion on an evaluation system of geothermal unit ranking and classification in China[J]. Earth Science Frontiers, 2017, 24(3):168-179.

[15]

王迪, 汪新伟, 毛翔, . 河北武城凸起地热田地热地质特征[J]. 地学前缘, 2020, 27(3):269-280.

[16]

WANG Di, WANG Xinwei, MAO Xiang, et al. Characteristics of geothermal geology of the Wucheng Uplift Geothermal field[J]. Earth Science Frontiers, 2020, 27(3):269-280.

[17]

曹瑛倬, 鲍志东, 鲁锴, . 冀中坳陷雄县地热田主控因素及成因模式[J]. 沉积学报, 2021, 39(4):863-872.

[18]

CAO Yingzhuo, BAO Zhidong, LU Kai, et al. Genetic model and main controlling factors of the Xiongan geothermal field[J]. Acta Sedimentologica Sinica, 2021, 39(4):863-872.

[19]

张英, 冯建贺, 何治亮, . 地热系统类型划分与主控因素分析[J]. 地学前缘, 2017, 24(3):190-198.

[20]

ZHANG Ying, FENG Jianyun, HE Zhiliang, et al. Classification of geothermal systems and their formation key factors[J]. Earth Science Frontiers, 2017, 24(3):190-198.

[21]

周总瑛, 刘世良, 刘金侠. 中国地热资源特点与发展对策[J]. 自然资源学报, 2015, 30(7):1210-1221.

[22]

ZHOU Zongying, LIU Shiliang, LIU Jinxia. Study on the characteristics and development strategies of geothermal resources in China[J]. Journal of Natural Resources, 2015, 30(7):1210-1221.

[23]

JAUPART C, LABROSSE S, LUCAZEAU F, et al.Temperatures, heat,and energy in the mantle of the Earth[J]. Earth Systems and Environmental Sciences, 2015,7:223-270.

[24]

王贵玲, 葡文静. 我国主要水热型地热系统形成机制与成因模式[J]. 地质学报, 2020, 94(7):1923-1937.

[25]

WANG Guiling, LIN Wenjing. Main hydro-geothermal systems and their genetic models in China[J]. Acta Geologica Sinica, 2020, 94(7):1923-1937.

[26]

陈志华, 刘运涛, 周称称, . 上蔡地热田地热开发利用潜力分析[J]. 中原工学院学报, 2021, 32(2):48-52.

[27]

CHEN Zhihua, LIU Yuntao, ZHOU Chengcheng, et al. Analysis of development and unilization potentiality of Shangcai geothermal field resources[J]. Journal of Zhongyuan University of Technology, 2021, 32(2):48-52.

[28]

白博文. 上蔡县地热资源成因分析及数值模拟研究[D]. 郑州: 郑州大学,2021:33-50.

[29]

BAI Bowen. Genesis and numerical simulation of geothermal resources in Shangcai County[D]. Zhengzhou: Zhengzhou University, 2021:33-50.

[30]

张天增, 刘运涛, 赵海军, . 驻马店市地热流体年龄研究[J]. 西部资源, 2013(3):155-158.

[31]

ZHANG Tianzeng, LIU Yuntao, ZHAO Haijun, et al. A study on the geothermal fluid age of Zhumadian City[J]. Western Resources, 2013(3):155-158.

[32]

赵鹏飞, 严永新, 杨香华. 舞阳凹陷始新统核桃园组物源示踪与砂体展布模式[J]. 海洋地质与第四纪地质, 2012, 32(3):37-44.

[33]

ZHAO Pengfei, YAN Yongxin, YANG Xianghua, et al. Provenance and distribution pattern of the sandbody of Eocene Hetaoyuan Formation in Wuyang Depression[J]. Marine Geology & Quaternary Geology, 2012, 32(3):37-44.

[34]

黄光寿, 郭丽丽, 黄凯. 河南省沉积盆地区五大构造单元地热地质特征[J]. 地质与资源, 2020, 29(2):172-179.

[35]

HUANG Guangshou, GUO Lili, HUANG Kai. Geothermal geological characteristics of five tectonic units in the sedimentary basins of Henan Provinc[J]. Geology and Resources, 2020, 29(2):172-179.

[36]

何争光. 周口坳陷古生界热演化史分析及其油气地质意义[D]. 西安: 西北大学,2009:10-12.

[37]

HE Zhengguang. The research of Palaeozoic thermal history and its oil-gas geological significance in Zhoukou Depression[D]. Xi'an: Northwest University,2009:10-12.

[38]

李杰, 张志强, 付越, . 不同热导率下 MIL-101(Cr)储氢过程的数值模拟研究[J]. 石油化工高等学校学报, 2023, 36(3):31-36.

[39]

LI Jie, ZHANG Zhiqiang, FU Yue, et al. Numerical simulation of hydrogen storage process in MIL-101(Cr)with different thermal conductivity[J]. Journal of Petrochemical Universities, 2023, 36(3):31-36.

[40]

于喜洹, 崔锡彪, 陆胜, . 早侏罗世粗中粒黑云母二长花岗岩岩石地球化学、LA-ICP-MS 锆石 U- Pb 年代学特征及成因:以大兴安岭北段潮满林场地区为例[J]. 东北石油大学学报, 2024, 48(2):27-41.

[41]

YU Xihuan, CUI Xibiao, LU Sheng, et al. Geochemistry and LA-ICP-MS zircon U-Pb chronology and genetic mechanism of the Early Jurassi ccoarseto medium grainedbiotite monzogranite:a case study of the Chaoman Forest Farm area in the Northern Great Xingan Range[J]. Journal of Northeast Petroleum University, 2024, 48(2):27-41.

[42]

王定一, 刘池洋, 张国伟, . 周口坳陷构造特征与油气远景[J]. 石油与天然气地质, 1991, 12(1):10-21.

[43]

WANG Dingyi, LIU Chiyang, ZHANG Guowei, et al. Structural feature and hydrocarbon potential of Zhoukou Depression[J]. Oil & Gas Geology, 1991, 12(1):10-21.

[44]

罗官幸, 潘虹, 李世宏, . 准噶尔盆地北三台凸起南斜坡石炭系火山岩储层特征及成藏模式[J]. 东北石油大学学报, 2024, 48(5): 27-47.

[45]

LUO Guanxing, PAN Hong, LI Shihong, et al. Reservoir characteristic sand reservoir forming model of Carboniferous volcanic rocks on the southern slope of Beisantai Uplift,Junggar Basin[J]. Journal of Northeast Petroleum University, 2024, 48(5):27-47.

[46]

佟子达, 张静, 周振菊, . 河南舞阳凹陷底部火山岩的发现及其锆石年代学和 Hf 同位素地球化学研究[J]. 大地构造与成矿学, 2016, 40(3):574-586.

[47]

TONG Zida, ZHANG Jing, ZHOU Zhenju, et al. Zircon U-Pb dating and Hf isotope compositions of the volcanic rocks from the bottom of the Wuyang Sag,Henan Province[J]. Geotectonica et Metallogenia, 2016, 40(3):574-586.

[48]

刘超, 付晓飞, 李扬成, . 烃源岩作为铀源岩的可能性:研究现状与展望[J]. 地学前缘, 2024, 31(2):284-298.

[49]

LIU Chao, FU Xiaofei, LI Yangcheng, et al. Can hydrocarbon source rock be uranium source rock:a review and prospectives[J]. Earth Science Frontiers, 2024, 31(2):284-298.

[50]

邬雪雁, 李进先. 河南省地壳结构和深断裂简述[J]. 河南地质, 1995, 13(2):126-131.

[51]

WU Xueyan, LI Jinxian. Discussing on crustal structure and deep faults of Henan Province[J]. Resources Guide, 1995, 13(2):126-131.

[52]

朱士波. 济阳坳陷热液流体活动特征及其油气地质意义[J]. 非常规油气, 2024, 11(2):21-28.

[53]

ZHU Shibo. Characteristics of hydrothermal fluid activity and its petroleum geological significance in Jiyang Depression[J]. Unconventional Oil & Gas, 2024, 11(2):21-28.

[54]

汪新伟, 高楠安, 王婷濒, . 河北献县地热田地热异常的分布特征及成因机制[J]. 地质学报, 2022, 96(7):2611-2625.

[55]

WANG Xinwei, GAO Nanan, WANG Tinghao, et al. Distribution characteristics and genetic mechanism of the geothermal abnormality in the Xianxian geothermal field,Hebei Province[J]. Acta Geologica Sinica, 2022, 96(7):2611-2625.

[56]

江晓雪, 朱传庆. 复杂热传递作用下冀中坳陷深、浅部地热资源差异分布[J/OL]. 地球科学,1-19[2024-07-18]. http://kns.cnki.net/ kcms/detail/42.1874.P.20240408.1659.025.html.

[57]

JIANG Xiaoxue, ZHU Chuanqing. Different distribution of deep and shallow geothermal resources in Jizhong Depression under complex heat transfer[J/OL]. Earth Science,1-19[2024-07-18]. http://kns.cnki.net/kcms/detail/42.1874.P.20240408.1659.025.html.

[58]

王迪, 国殿斌, 汪新伟, . 河南清丰地区岩溶热储地热地质特征[J]. 东北石油大学学报, 2020, 44(1):32-43.

[59]

WANG Di, GUO Dianbin, WANG Xinwei, et al. Characteristics of geothermal geology of karst geothermal reservoir in Qingfeng Area,Henan[J]. Journal of Northeast Petroleum University, 2020, 44(1):32-43.

[60]

姜光政, 高明, 饶松, . 中国大陆地区大地热流数据汇编:第四版[J]. 地球物理学报, 2016, 59(8):2892-2910.

[61]

JIANG Guangzheng, GAO Peng, RAO Song, et al. Compilation of heat flow data in the continental area of China:4th edition[J]. Chinses Journal of Geophysics, 2016, 59(8):2892-2910.

[62]

杨义栋, 刘彦兵, 赵盼, . 周口凹陷区地温场特征及影响因素分析[J]. 中国矿业, 2021, 30(3):231-236.

[63]

YANG Yidong, LIU Yanbing, ZHAO Pan, et al. Analysis of geothermal field characteristics and influencing factors in Zhoukou Depression area[J]. China Mining Magazine, 2021, 30(3):231-236.

[64]

孙家振, 韦必则, 熊保贤, . 周口坳陷形成机制及其与大别造山带的辐合关系[J]. 地学前缘, 1995, 2(3/4):248-251.

[65]

SUN Jiazhen, WEI Bize, XIONG Baoxian, et al. The formation mechanism of Zhoukou Depression and its convergence relationship with the Dabie Orogenic Belt[J]. Earth Science Frontiers, 1995, 2(3/4):248-251.

[66]

张英杰, 王龙. 显生宙一级层序的银河年旋回响应:重要的进展与争论[J]. 地球科学进展, 2020, 35(3):275-285.

[67]

ZHANG Yingjie, WANG Long. Response of first-order sequence to the galactic year cycle in the Phanerozoic:an important progress and topic[J]. Advances in Earth Science, 2020, 35(3):275-285.

[68]

刘志武, 周立发, 何明喜. 周口坳陷石炭一二叠纪残留盆地煤成油气勘探前景[J]. 新疆石油地质, 2008, 29(6):699-702.

[69]

LIU Zhiwu, ZHOU Lifa, HE Mingxi. Prospects for coal formed oil and gas exploration of Carboniferous-Permian residual basins in Zhoukou Depression[J]. Xinjiang Petroleum Geology, 2008, 29(6):699-702.

[70]

周颖, 杜利, 魏广仁, . 南华北南缘长山隆起斜坡带寒武系岩溶地热资源特征[J]. 石化技术, 2023, 30(9):184-186.

[71]

ZHOU Ying, DU Li, WEI Guangren, et al. Characteristics of Cambrian karst geothermal resources in the slope zone of Changshan Uplift in the southern margin of Southern North China Basin[J]. Petrochemical Technology, 2023, 30(9):184-186.

[72]

田禹. 鲁东地热区氢氧同位素特征及地热水补给来源[J]. 地质科技情报, 2015, 34(6):182-185.

[73]

TIAN Yu. Features of hydrogen and oxygen isotopes and the make-up source for geothermal water in East Shandong geothermal area[J]. Geological Science and Technology Information, 2015, 34(6):182-185.

[74]

赵晨旭, 李忠诚, 郭世超, . 松辽盆地南部长岭断陷青一段陆相页岩地球化学和沉积环境特征[J]. 特种油气藏, 2023, 30(6):55-61.

[75]

ZHAO Chenxu, LI Zhongcheng, GUO Shichao, et al. Characteristics of geochemistry and depositional environment of terrestrial shales in the first member of Qingshankou Formation of Changling Fault Depression in the Southern Songliao Basin[J]. Special Oil & Gas Reservoirs, 2023, 30(6):55-61.

[76]

郭飒飒, 朱传庆, 邱楠生, . 雄安新区深部地热资源形成条件与有利区预测[J]. 地质学报, 2020, 94(7):2026-2035.

[77]

GUO Sasa, ZHU Chuanqing, QIU Nansheng, et al. Formation conditions and favorable areas for the deep geothermal resources in the Xionǵan Area[J]. Acta Geologica Sinica, 2020, 94(7):2026-2035.

[78]

黄禄渊, 杨树新, 崔效锋, . 华北地区实测应力特征与断层稳定性分析[J]. 岩土力学, 2013, 34(增刊1):204-213.

[79]

HUANG Luyuan, YANG Shuxin, CUI Xiaofeng, et al. Analysis of characteristics of measured stress and stability of faults in North China[J]. Rock and Soil Mechanics, 2013,34 (Supp.1):204-213.

基金资助

中国石油西南油气田分公司项目(XNS-JS2024-02)

AI Summary AI Mindmap
PDF (20963KB)

0

访问

0

被引

详细

导航
相关文章

AI思维导图

/