“

本次服务由安徽南国冷热综合能源有限公司（点击了解详情）冠名赞助

该公司主要业务范围为：区域集中供冷供暖智慧运营、能源互联网、建筑及工业节能、数据中心供冷及应急冷源建设、集成电路无尘车间、手术室实验室净化工程、中央空调工程、智能化工程、信息化系统集成等高新技术服务。

作者 | 李文靖 肖红平 饶松 施亦做 张翘然 黄顺德 胡光明

标题 | 松辽盆地中央坳陷及邻区三维地热地质建模与地热资源靶区优选

来源 | 地质科学

编辑 | 地热小芯（添加微信号:geothermalAI,可获得相关资料）

→这是地热能在线AI地热小芯编辑的第1篇文章

01

全文导读

在地热资源勘探领域，三维地热地质建模技术的应用日益成为研究热点。近期，科研人员利用地球物理、钻孔资料以及岩石热物性数据，采用3D Geomodeller软件的空间插值方法，成功构建了松辽盆地中央坳陷区及其邻近地区的三维地热地质模型。该模型不仅直观展现了地质体的温度场分布，而且为确定地热资源的有利开发区域提供了重要依据。

通过对比盲井地层分层和钻孔实测温度数据，研究人员验证了三维地热地质建模和温度场模拟的准确性。研究结果显示，松辽盆地中央坳陷区及其邻区在1.0至4.0公里深度的地层温度分别在30.3℃至62.8℃、68.2℃至120.2℃、110.5℃至166.7℃、158.4℃至214.2℃之间。地温场的高异常区主要集中在大庆长垣中部、宾县王府凹陷和长春岭背斜带。

此外，研究还发现嫩江组、姚家组二段—三段、青山口组二段—三段、泉三段—四段四套主力热储层底板温度分别介于15.8℃至71.4℃、23.6℃至88.6℃、31.8℃至107.4℃、48.9℃至133.4℃之间，其中华字井阶地、大庆长垣、宾县王府凹陷为主力热储温度的高值区。

研究指出，现今研究区的地温场分布特征主要受基底起伏的控制。基底和沉积层热导率的差异导致的热流“折射”效应，促进了浅部热量的再分配，形成了凹凸相间的热流分布格局。断裂构造对地温场高异常区的分布也有显著影响。

综合分析热源、通道和储盖组合特征后，研究人员圈定了大庆长垣中部地区泉头组三段—四段作为松辽盆地中央坳陷地热资源开发的有利靶区，为未来的地热资源开发提供了科学指导。

02

HIGHLIGHT图片

图1 松辽盆地中央坳陷及邻区钻孔和地震剖面分布位置及地层剖面图（据 Ryder et al.,2003 修改）

Fig.1 Distribution location and stratigraphic profile of boreholes and seismic sections in the central depression and adjacent areas of the Songliao Basin(modified from Ryder et al.,2003 )

图2 松辽盆地中央坳陷及邻区三维地热地质建模及地温场模拟流程图（据 Calcagno et al.,2014 修改）

Fig.2 Flow chart of three-dimensional geothermal geological modeling and geothermal field simulation in the central depression and adjacent areas of Songliao Basin(modified from Calcagno et al.,2014 )

图3 松辽盆地中央坳陷及邻区三维地热地质模型

Fig.3 A three-dimensional geothermal geological model of the central depression and adjacent areas in the Songliao Basin

图4 源292、古514井分层数据和模型分层数据对比

Fig.4 Comparison of stratified data and model stratified data of Yuan 292 and Gu 514 wells

图5 徐深1和松科2实测与模拟地温曲线对比

Fig.5 Comparison of measured and simulated ground temperature curves between Xushen 1 and Songke 2

图6 松辽盆地中央坳陷及邻区实测与模拟热流值拟合图

Fig.6 Fitting diagram of measured and simulated heat flow values in the central depression and adjacent areas of the Songliao Basin

图7 松辽盆地中央坳陷及邻区不同深度地温场模拟结果

Fig.7 Simulation results of geothermal fields at different depths in the central depression and adjacent areas of the Songliao Basin

图8 松辽盆地中央坳陷及邻区0～4.0 km深度平均地温梯度平面展布

Fig.8 Plane distribution of average geothermal gradient at a depth of0～4.0 km in the central depression and adjacent areas of the Songliao Basin

图9 松辽盆地中央坳陷及邻区主力热储底板温度平面展布

Fig.9 Temperature distribution of the main thermal storage floor in the central depression and adjacent areas of the Songliao Basin

图1 0 松辽盆地sl2、sl5地震剖面地温场模拟结果（剖面位置见图1)

Fig.10 Simulation results of ground temperature field in seismic sections sl2 and sl5 of the Songliao Basin(profile shown in Fig.1)

图1 1 松辽盆地中央坳陷及邻区150.0℃等温面埋深等值线图

Fig.11 Contour map of 150.0℃isothermal surface burial depth in the central depression and adjacent areas of the Songliao Basin

免责声明：本文仅用于学术交流和传播，不构成投资建议

——-

参考资料：

付健,李思其,贾小江等.2023.松辽盆地中央坳陷区中—新生代岩石圈厚度演化.地质科学,58(3):798-809.Fu Jian,Li Siqi,Jia Xiaojiang et al.2023.Mesozoic-Cenozoic lithospheric thickness evolution in the central depression of Songliao Basin.Chinese Journal of Geology, 58(3):798-809.

韩江涛,郭振宇,刘文玉等.2018.松辽盆地岩石圈减薄的深部动力学过程.地球物理学报,61(6):2265-2279.Han Jiangtao,Guo Zhenyu,Liu Wenyu et al.2018.Deep dynamic process of lithosphere thinning in Songliao Basin.Chinese Journal of Geophysics,61(6):2265-2279.

韩湘君,金旭.2002.中国东北地区地热资源及热结构分析.地质与勘探,38(1):74-76.Han Xiangjun and Jin Xu.2002.Geothermal resource and thermail structure in northeastern China.Geology and Exploration,38(1):74-76.

胡望水,吕炳全,张文军等.2005.松辽盆地构造演化及成盆动力学探讨.地质科学,40(1):16-31.Hu Wangshui,LüBingquan,Zhang Wenjun et al.2005.An approach to tectonic evolution and dynamics of the Songliao Basin.Chinese Journal of Geology,40(1):16-31.

黄磊,童亨茂,杨东辉等.2019.松辽盆地大庆长垣中浅层断层形成演化的新模式.地质学报,93(3):597-605.Huang Lei,Tong Hengmao,Yang Donghui et al.2019.A new model for the formation and evolution of middle-shallow faults in the Daqing placanticline,Songliao Basin.Acta Geologica Sinica,93(3):597-605.

姜光政,高堋,饶松等.2016.中国大陆地区大地热流数据汇编(第四版).地球物理学报,59(8):2892-2910.Jiang Guangzheng,Gao Peng,Rao Song et al.2016.Compilation of heat flow data in the continental area of China(4th Edition).Chinese Journal of Geophysics,59(8):2892-2910.

康凤新,赵季初,黄迅等.2023.华北盆地梁村古潜山岩溶热储聚热机制及资源潜力.地球科学,48(3):1080-1092.Kang Fengxin,Zhao Jichu,Huang Xun et al.2023.Heataccumulation mechanism and resources potential of the karst geothermal reservoir in Liangcun buried uplift of Linqing Depression.Earth Science,48(3):1080-1092.

雷振宇,解习农,孟元林等.2013.松辽盆地北部中央坳陷带异常压力条件下地层水化学特征及其成岩响应.石油实验地质,35(1):81-86.Lei Zhenyu,Xie Xinong,Meng Yuanlin et al.2013.Chemical features and diagenesis reactions of formation water under abnormal pressure in central depression of northern Songliao Basin.Petroleum Geology&Experiment,35(1):81-86.

李志安.1995.松辽盆地地幔热流的演化特征.大地构造与成矿学,19(2):104-112.Li Zhian.1995.Evolutionary features of mantle heat flux in Songliao Basin.Geotectonica et Metallogenia,19(2):104-112.

蔺文静,刘志明,王婉丽等.2013.中国地热资源及其潜力评估.中国地质,40(1):312-321.Lin Menjing,Liu Zhiming,Wang Wanli et al.2013.The assessment of geothermal resources potential of China.Geology in China,40(1):312-321.

刘雨晨,柳波,朱焕来等.2023.松辽盆地现今地温场分布特征及主控因素.地质学报,97(8):2715-2727.Liu Yuchen,Liu Bo,Zhu Huanlai et al.2023.The distribution characteristics and main controlling factors of present-day geothermal regime of the Songliao Basin.Acta Geologica Sinica,97(8):2715-2727.

牛璞,韩江涛,曾昭发等.2021.松辽盆地北部地热场深部控制因素研究:基于大地电磁探测的结果.地球物理学报,64(11):4060-4074.Niu Pu,Han Jiangtao,Zeng Zhaofa et al.2021.Deep controlling factors of the geothermal field in the northern Songliao Basin derived from magnetotelluric survey.Chinese Journal of Geophysics,64(11):4060-4074.

庞忠和,黄少鹏,胡圣标等.2014.中国地热研究的进展与展望(1995~2014).地质科学,49(3):719-727.Pang Zhonghe,Huang Shaopeng,Hu Shengbiao et al.2014.Geothermal studies in China:Progress and prospects1995-2014.Chinese Journal of Geology,49(3):719-727.

庞忠和,孔彦龙,庞菊梅等.2017.雄安新区地热资源与开发利用研究.中国科学院院刊,32(11):1224-1230.Pang Zhonghe,Kong Yanlong,Pang Jumei et al.2017.Geothermal resources and development in Xiong’an New Area.Bulletin of Chinese Academy of Sciences,32(11):1224-1230.

邱楠生,魏刚,李翠翠等.2009.渤海海域现今地温场分布特征.石油与天然气地质,30(4):412-419.Qiu Nansheng,Wei Gang,Li Cuicui et al.2009.Distribution features of current geothermal field in the Bohai Sea waters.Oil&Gas Geology,30(4):412-419.

邱楠生,唐博宁,朱传庆.2022.中国大陆地区温泉分布的深部热背景.地质学报,96(1):195-207.Qiu Nansheng,Tang Boning and Zhu Chuanqing.2022.Deep thermal background of hot spring distribution in the Chinese continent.Acta Geologica Sinica,96(1):195-207.

饶松,高腾,肖红平等.2022.中国油区地热开发利用进展.科技导报,40(20):65-75.Rao Song,Gao Teng,Xiao Hongping et al.2022.Progress and prospective of geothermal exploitation and utilization in oil fields of China.Science&Technology Review,40(20):65-75.

施亦做,王社教,肖红平等.2022.基于三维地质建模的松辽盆地北部地温场模拟.天然气工业,42(4):46-53.Shi Yizuo,Wang Shejiao,Xiao Hongping et al.2022.3D GeoModeller-based simulation of the geothermal field in the northern Songliao Basin.Nature Gas Industry,42(4):46-53.

孙雨,于利民,闫百泉等.2018.松辽盆地三肇凹陷向斜区白垩系姚家组葡萄花油层油水分布特征及其主控因素.石油与天然气地质,39(6):1120-1130.Sun Yu,Yu Limin,Yan Baiquan et al.2018.Oil-water distribution and its major controlling factors of Putaohua reservoir of the Cretaceous Yaojia Formation in syncline area of Sanzhao Sag,Songliao Basin.Oil&Gas Geology,39(6):1120-1130.

索艳慧,李三忠,曹现志等.2017.中国东部中新生代反转构造及其记录的大洋板块俯冲过程.地学前缘,24(4):249-267.Suo Y anhui,Li Sanzhong,Cao Xianzhi et al.2017.Mesozoic-Cenozoic inversion tectonics of East China and its implications for the subduction process of the oceanic plate.Earth Science Frontiers,24(4):249-267.

谭世燕,石义强,赵育捷.2001.松辽盆地地热资源的形成与远景评价.世界地质,20(2):155-160.Tan Shiyan,Shi Yiqiang and Zhao Yujie.2001.The formation and prospective evaluation of geothermal resources in the Songliao Basin.World Geology,20(2):155-160.

田有,马锦程,刘财等.2019.西太平洋俯冲板块对中国东北构造演化的影响及其动力学意义.地球物理学报,62(3):1071-1082.Tian You,Ma Jincheng,Liu Cai et al.2019.Effects of subduction of the western Pacific Plate on tectonic evolution of Northeast China and geodynamic implications.Chinese Journal of Geophysics,62(3):1071-1082.

汪集旸,胡圣标,庞忠和等.2012.中国大陆干热岩地热资源潜力评估.科技导报,30(32):25-31.Wang Jiyang,Hu Shengbiao,Pang Zhonghe et al.2012.Estimate of geothermal resources potential for hot dry rock in the continental area of China.Science&Technology Review,30(32):25-31.

汪集暘.2015.地热学及其应用.北京:科学出版社.1-548.Wang Jiyang.2015.Geothermics and Its Applications.Beijing:Science Press.1-548.

汪集暘,邱楠生,胡圣标等.2017.中国油田地热研究的进展和发展趋势.地学前缘,24(3):1-12.Wang Jiyang,Qiu Nansheng,Hu Shengbiao et al.2017.Advancement and developmental trend in the geothermics of oil fields in China.Earth Science Frontiers.24(3):1-12.

汪在君.2003.松辽盆地北部的地热资源及其开发利用方向.自然资源学报,18(1):8-12.Wang Zaijun.2003.The geothermal resource of the northern Songliao Basin and direction for its development and utilization.Journal of Natural Resources,18(1):8-12.

王贵玲,马峰,侯贺晟等.2023.松辽盆地坳陷层控地热系统研究.地球学报,44(1):21-32.Wang Guiling,Ma Feng,Hou Hesheng et al.2023.Study of depression and layer controlled geothermal system in Songliao Basin.Acta Geoscientica Sinica,44(1):21-32.

王社教,闫家泓,黎民等.2014.油田地热资源评价研究新进展.地质科学,49(3):771-780.Wang Shejiao,Yan Jiahong,Li Min et al.2014.New advances in the study of oilfield geothermal resources evaluation.Chinese Journal of Geology,49(3):771-780.

张健,方桂,何雨蓓.2023a.中国东部地热异常区深层高温分布特征与动力学背景.地学前缘,30(2):316-332.Zhang Jian,Fang Gui and He Yubei.2023a.High-temperature characteristics and geodynamic background at depth of geothermal anomaly areas in eastern China.Earth Science Frontiers,30(2):316-332.

张健,何雨蓓,范艳霞.2023b.松辽盆地地壳热结构与深部热源条件.地球科学与环境学报,45(2):157-167.Zhang Jian,He Yubei and Fan Yanxia.2023b.Crustal thermal structure and deep heat source conditions in Songliao Basin,NE China.Journal of Earth Sciences and Environment,45(2):157-167.

张翘然,肖红平,饶松等.2023.松辽盆地现今地温场特征及控制因素.地质科技通报,1-14.网络首发.Zhang Qiaoran,Xiao Hongping,Rao Song et al.2023.Characteristics and controlling factors of present geothermal field in the Songliao Basin.Bulletin of Geological Science and Technology,1-14.Publish Online.

翟志伟,施尚明,朱焕来.2011.大庆长垣西部地区地热资源潜力分布.科学技术与工程,11(4):834-837.Zhai Zhiwei,Shi Shangming and Zhu Huanlai.2011.Potential distribution of geothermal resource in western region of Daqing Placanticline.Science Technology and Engineering,11(4):834-837.

赵波,尹淑敏,张顺等.2009.松辽盆地中央坳陷滨北地区上白垩统青山口组沉积相与沉积演化.古地理学报,11(3):293-300.Zhao Bo,Yin Shumin,Zhang Shun et al.2009.Sedimentary facies and sedimentary evolution of the Upper Cretaceous Qingshankou Formation of Binbei area in central depression of Songliao Basin.Journal of Palaeogeography,11(3):293-300.

朱焕来.2011.松辽盆地北部沉积盆地型地热资源研究(博士学位论文).黑龙江大庆:东北石油大学.1-104.Zhu Huanlai.201 1.Research on the Sedimentary Geothermal Resources in North Songliao Basin(PhD Thesis).Daqing,Heilongjiang:Northeast Petroleum University.1-104.

朱筱敏,刘媛,方庆等.2012.大型坳陷湖盆浅水三角洲形成条件和沉积模式:以松辽盆地三肇凹陷扶余油层为例.地学前缘,19(1):89-99.Zhu Xiaomin,Liu Yuan,Fang Qing et al.2012.Formation and sedimentary model of shallow delta in large-scale lake:Example from Cretaceous Quantou Formation in Sanzhao Sag,Songliao Basin.Earth Science Frontiers,19(1):89-99.

Calcagno P,Baujard C,Guillou-Ftottier L et al.2014.Estimation of the deep geothermal potential within the Tertiary Limagne Basin(French massif central):An integrated 3D geological and thermal approach.Geothermics,51:496-508.DOI:10.1016/j.geothermics.2014.02.002.

Chen L,Berntsson F,Zhang Z J et al.2014.Seismically constrained thermo-rheological structure of the eastern Tibetan margin:Implication for lithospheric delamination.Tectonophylics,627:122-134.DOI:10.1016/j.tecto.2013.11.005.

Jiang G Z,Tian Y T,Lv Q T et al.2023.Ground surface temperature history since the Last Glacial Maximum in Northeast Asia:Reconstructions from the borehole geotherms of the International Continental Scientific Drilling Program.Geophysical Research Letters,50(8):e2023GL1 03055.DOI:10.1029/2023GL103055.

Lachenbruch A H and Sass J H.1977.Heat flow in the United States and the thermal regime of the crust.//Heacock J G,Keller G V,Oliver J E et al.The Earth’s Crust.Washington:American Geophysical Union.626-675.DOI:10.1029/GM020p0626.

Magnabosco R,Galvão P and De Carvalho A M.2020.An approach to map karst groundwater potentiality in an urban area,Sete Lagoas,Brazil.Hydrological Sciences Journal,65(14):2482-2498.DOI:10.1080/02626667.2020.1802031.

Mottaghy D,Pechnig R and Vogt C.2011.The geothermal project Den Haag,3D numerical models for temperature prediction and reservoir simulation.Geothermics,40(3):199-210.DOI:10.1016/j.geothermics.2011.07.001.

Qiu N S,Xu W,Zuo Y H et al.2015.Meso-Cenozoic thermal regime in the Bohai Bay Basin,eastern North China Craton.International Geology Review,57(3):271-289.DOI:10.1080/00206814.2014.1002818.

Ryder R T,Qiang J,McCabe P J et al.2003.Qingshankou-Putaohua/Shaertu and Jurassic coal-Denglouku/Nongan total petroleum systems in the Songliao Basin,China.U.S.Geological Survey Bulletin,2203-A:1-24.DOI:10.3133/B 2203A.

Shi Y Z,Jiang G Z,Zhang X Y et al.2019.Present temperature field characterization and geothermal resource assessment in the Harbin area,Northeast China.Energy Exploration&Exploitation,37(2):834-848.DOI:10.1177/0144598718815922.

Shi Y Z,Jiang G Z,Shi S M et al.2022.Terrestrial heat flow and its geodynamic implications in the northern Songliao Basin,Northeast China.Geophysical Journal International,229(2):962-983.DOI:10.1093/gji/ggab500.

Siekel R,Stüwe K,Gibson H et al.2009.Forward prediction of spatial temperature variation from 3D geology models.ASEG Extended Abstracts,2009(1):1-9.DOI:10.1071/ASEG2009ab117.

Teng Y,Koike K.2007.Three-dimensional imaging of a geothermal system using temperature and geological models derived from a well-log dataset.Geothermics,36(6):518-538.DOI:10.1016/j.geothermics.2007.07.006.

Wang S J,Yan J H,Li F et al.2016.Exploitation and utilization of oilfield geothermal resources in China.Energies,9(10):798.DOI:10.3390/en9100798.

Yang W Y,Xiao C L,Zhang Z H et al.2022.Identification of the formation temperature field of the southern Songliao Basin,China based on a deep belief network.Renewable Energy,182:32-42.DOI:10.1016/j.renene.2021.09.127.