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渤海盆地秦南凹陷新生代以来构造-热演化史

高玉飞 唐晓音 杨树春 赵欣妍 胡圣标

地质力学学报2024,Vol.30Issue(4):622-632,11.
地质力学学报2024,Vol.30Issue(4):622-632,11.DOI:10.12090/j.issn.1006-6616.2023168

渤海盆地秦南凹陷新生代以来构造-热演化史

Cenozoic tectonic-thermal history reconstruction of the Qinnan Depression,Bohai Basin

高玉飞 1唐晓音 2杨树春 1赵欣妍 2胡圣标3

作者信息

  • 1. 中海油研究总院,北京 100027
  • 2. 中国地质科学院地质力学研究所,北京 100081||自然资源部古地磁与古构造重建重点实验室,北京 100081||中国地质调查局油气地质力学重点实验室,北京 100081
  • 3. 中国科学院地质与地球物理研究所,北京 100029
  • 折叠

摘要

Abstract

[Objective]Tectono-thermal history is important to understand basin evolution and its geodynamic mechanism and is the key question to be solved for source rock maturation study.With the increasing energy demand and difficulty in oil and gas discovery on land,sea basins have gradually become an important alternative for oil and gas exploration and a hotspot of national energy strategy research.The Qinnan Depression,located in the northwest of the Bohai Sea,has good exploration prospects.However,owing to the low level of exploration,research on the tectono-thermal evolution of Qinnan Depression is still limited.[Methods]In this study,25 artificial wells have been established based on 3 seismic profiles of the Qinnan Depression,and their tectonic subsidence and thermal history have been modeled to reconstruct the tectonic-thermal evolution history using a multi-stage finite stretching model.[Results]The results indicate that since the Cenozoic era,the Qinnan Depression has undergone three stages of rifting and stretching during the sedimentary periods of the Kongdian Formation to fourth member of the Shahejie Formation(65-42 Ma),the third member of the Shahejie Formation(42-38 Ma),and the third member of the Dongying Formation(32.8-30.3 Ma),with a total stretching factor of 1.27-2.05.Corresponding to the three stages of stretching,the basal heat flow of the Qinnan Depression has experienced three stages of increase,reaching a peak of 64.0-89.0 mW/m2 at the end of the deposition of the third member of the Dongying Formation(~30.3 Ma),and then decreased gradually until present.[Conclusion]The Qinnan Depression underwent three phases of heating and two stages of cooling since the Cenozoic period.There is a good coupling relationship between the tectonic-thermal evolution process and fault activity in the Qinnan Depression.[Significance]The parameters such as tension system and basement heat flow history obtained in this study are of great significance for understanding the deep dynamic mechanisms of basin tectonic evolution and guiding oil and gas exploration.

关键词

渤海盆地/秦南凹陷/构造沉降/热史演化/新生代

Key words

Bohai Basin/Qinnan Depression/structure subsidence/thermal history/Cainozoic

分类

天文与地球科学

引用本文复制引用

高玉飞,唐晓音,杨树春,赵欣妍,胡圣标..渤海盆地秦南凹陷新生代以来构造-热演化史[J].地质力学学报,2024,30(4):622-632,11.

基金项目

国家自然科学基金项目(42072181) (42072181)

中海石油有限公司科研项目(YXKY-ZX 01 2021) This research is financially supported by the National Natural Science Foundation of China(Grant No.42072181)and the CNOOC Research Project"Resource Potential,Reservoir Formation Mechanism and Breakthrough Direction of Potential Oil-rich Depressions in Offshore Basins of China"(Grant No.YXKY-ZX 01 2021). (YXKY-ZX 01 2021)

地质力学学报

OA北大核心CSTPCD

1006-6616

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