南黄海盆地地层生热率及岩石圈热结构

孙旭东; 郭兴伟; 张训华; 李子渊; 刘怀山; 张升升

doi:10.3799/dqkx.2023.044

Volume 48 Issue 3

Mar. 2023

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Sun Xudong, Guo Xingwei, Zhang Xunhua, Li Ziyuan, Liu Huaishan, Zhang Shengsheng, 2023. Radiogenic Heat Production of Formation and Thermal Structure of Lithosphere in the South Yellow Sea Basin. Earth Science, 48(3): 1040-1057. doi: 10.3799/dqkx.2023.044

Citation:

Sun Xudong, Guo Xingwei, Zhang Xunhua, Li Ziyuan, Liu Huaishan, Zhang Shengsheng, 2023. Radiogenic Heat Production of Formation and Thermal Structure of Lithosphere in the South Yellow Sea Basin. Earth Science, 48(3): 1040-1057. doi: 10.3799/dqkx.2023.044

Citation:

Sun Xudong, Guo Xingwei, Zhang Xunhua, Li Ziyuan, Liu Huaishan, Zhang Shengsheng, 2023. Radiogenic Heat Production of Formation and Thermal Structure of Lithosphere in the South Yellow Sea Basin. Earth Science, 48(3): 1040-1057. doi: 10.3799/dqkx.2023.044

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Radiogenic Heat Production of Formation and Thermal Structure of Lithosphere in the South Yellow Sea Basin

doi: 10.3799/dqkx.2023.044

Sun Xudong^{1, 2, 3
,
,},
Guo Xingwei^{2, 3
,
,},
Zhang Xunhua^{1, 2, 3},
Li Ziyuan⁴,
Liu Huaishan¹,
Zhang Shengsheng^{1, 2, 3}

1.
College of Marine Geoscience, Ocean University of China, Qingdao 710069, China
2.
Qingdao Institute of Marine Geology, Qingdao 266071, China
3.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
4.
PetroChina Co. Ltd., Petrochina Southwest Oil and Gas Field Company South Sichuan Gas District, Luzhou 646001, China

Received Date: 2022-04-30
Available Online: 2023-03-27
Publish Date: 2023-03-25

Abstract

Abstract

The study of lithosphere thermal structure state can not only understand the deep dynamic evolution mechanism of the lithosphere, but also be an important part of the evaluation of oil and gas resources in oil-bearing areas. The lack of heat generation rate data in the South Yellow Sea basin gets in the way of the research progress of lithospheric thermal structure. In this paper, the heat generation rate of sedimentary strata in the South Yellow Sea basin is calculated by the empirical relationship of GR (gamma value)-A (rock heat generation rate). Under the constraints of the terrestrial heat flow, the formation heat generation rate, the two-dimensional multi-channel seismic profile that passes through the basin in the south-north direction and the crust velocity structure profile OBS2013, the crust heat generation model of the South Yellow Sea basin was established, and the lithospheric thermal structure of the basin was calculated. The calculated results of lithospheric thermal structure show that: (1) the Moho average temperature of the three sub-units of the north depression, the central uplift and the south depression of the South Yellow Sea basin are 602.2±15.25 ℃, 592.7±2.56 ℃ and 650.6±20.24 ℃, respectively; (2) The average thermal lithosphere thickness is 99.7±2.20 km, 101.7±0.51 km, 88.2±2.49 km; (3) The crust-mantle heat flux ratios are 0.76±0.02, 0.88±0.01, and 0.71±0.15, respectively, with the characteristics of "cold crust and hot mantle". The results of this paper reveal that the South Yellow Sea basin not only has a high heat flow background, but also is in the transition stage from tectonic active area to tectonic stable area. In addition, the different lithospheric thermal structure characteristics of the three sub-units in the present South Yellow Sea basin may be related to the tectonic setting of the para-foreland basin formed on the south side of the Sulu orogenic belt (present northern depression) by the subduction collision of the Yangtze block and the North China block in the Late Triassic.
- South Yellow Sea basin,
- natural gamma value,
- heat generation rate of rock,
- thermal structure of lithosphere,
- thermal thickness of lithosphere,
- geothermal energy

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References(90)

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Radiogenic Heat Production of Formation and Thermal Structure of Lithosphere in the South Yellow Sea Basin

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