IGGCAS OpenIR  > 岩石圈演化国家重点实验室
Terrestrial heat flow and its geodynamic implications in the northern Songliao Basin, Northeast China
Shi, Yizuo1; Jiang, Guangzheng2; Shi, Shangming3; Wang, Zecheng1; Wang, Shejiao1; Wang, Zhuting4; Hu, Shengbiao5
2022-01-31
Source PublicationGEOPHYSICAL JOURNAL INTERNATIONAL
ISSN0956-540X
Volume229Issue:2Pages:962-983
AbstractHeat flow data are essential for understanding lithospheric dynamics. As a petroliferous basin, a large number of boreholes have been drilled during hydrocarbon exploration and production in the northern part of Songliao Basin, Northeast China. Meanwhile, the data on crustal structures, core samples and formation temperatures have been accumulated, which provide an opportunity for understanding the thermal state of the basin. Based on the temperature data from both Drilling Stem Test and continuous steady-state logging profiles, together with the systematic analysis of the thermal properties of rock samples, we present a new heat flow map of the northern Songliao Basin with significantly increased number of heat flow sites. The northern Songliao Basin is characterized by relatively high geothermal gradients and high heat flow for sedimentary basins. The heat flow values range from 44.4 to 95.0 mW m(-2) with an average of 67.2 +/- 12.8 mW m(-2), and the geothermal gradients range from 21 to 59 degrees C km(-1) with an overall average of 41.7 degrees C km(-1). Heat production from sedimentary covers accounts for about 4.5 mW m(-2) at the site of Well SK-2. Furthermore, based on the crustal structures revealed by previous seismic studies, lithospheric thermal structures are analysed and compared among different structural units of the basin. A thinned thermal lithosphere with a thickness of similar to 65 km is found beneath the Central downwarp and the Southeast uplift in which a large part of the heat flow is mantle derived. The Western Slope exhibits a moderate heat flow value and a thicker thermal lithosphere with thickness greater than 110 km. From the perspective of the geothermal state of the lithosphere, the regional geodynamics related to the Mesozoic lithosphere stretching and the subduction of the Pacific Plate are discussed.
KeywordHeat flow Heat generation and transport Sedimentary basin processes Composition and structure of the continental crust Dynamics of lithosphere and mantle Asia
DOI10.1093/gji/ggab500
Funding OrganizationNational Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; PetroChina Company Limited ; PetroChina Company Limited ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; PetroChina Company Limited ; PetroChina Company Limited ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; PetroChina Company Limited ; PetroChina Company Limited ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; PetroChina Company Limited ; PetroChina Company Limited
Language英语
Funding ProjectNational Natural Science Foundation of China (NSFC)[42102339] ; PetroChina Company Limited[2021DJ5501]
Funding OrganizationNational Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; PetroChina Company Limited ; PetroChina Company Limited ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; PetroChina Company Limited ; PetroChina Company Limited ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; PetroChina Company Limited ; PetroChina Company Limited ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; PetroChina Company Limited ; PetroChina Company Limited
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics
WOS IDWOS:000763003500005
PublisherOXFORD UNIV PRESS
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/104992
Collection岩石圈演化国家重点实验室
Corresponding AuthorShi, Yizuo
Affiliation1.CNPC, Res Inst Petr Explorat & Dev, Beijing 100081, Peoples R China
2.Chengdu Univ Technol, Coll Energy, Chengdu 610059, Sichuan, Peoples R China
3.Northeast Petr Univ, Sch Earth Sci, Daqing 163318, Heilongjiang, Peoples R China
4.China Univ Min & Technol, Sch Mines, Xuzhou 221116, Jiangsu, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
Recommended Citation
GB/T 7714
Shi, Yizuo,Jiang, Guangzheng,Shi, Shangming,et al. Terrestrial heat flow and its geodynamic implications in the northern Songliao Basin, Northeast China[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2022,229(2):962-983.
APA Shi, Yizuo.,Jiang, Guangzheng.,Shi, Shangming.,Wang, Zecheng.,Wang, Shejiao.,...&Hu, Shengbiao.(2022).Terrestrial heat flow and its geodynamic implications in the northern Songliao Basin, Northeast China.GEOPHYSICAL JOURNAL INTERNATIONAL,229(2),962-983.
MLA Shi, Yizuo,et al."Terrestrial heat flow and its geodynamic implications in the northern Songliao Basin, Northeast China".GEOPHYSICAL JOURNAL INTERNATIONAL 229.2(2022):962-983.
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