ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
基于测井频谱分析的松科二井登娄库组地层沉积速率研究
  
关键词:CCSD SK-2  Denglouku Formation  geophysical logs  sedimentation rate  astronomical cycle
基金项目:中国地质调查局地质调查专项(编号: 1212011301600);国家自然科学基金委重大项目专题(编号: 41790455-1);中央高校基本科研业务费专项资金资助项目(编号: 2652019003)
作者单位E-mail
张浩东 中国地质大学(北京)地下信息探测技术与仪器教育部重点实验室
中国地质大学(北京)地球物理与信息技术学院 
2754614535@qq.com 
邹长春 中国地质大学(北京)地下信息探测技术与仪器教育部重点实验室
中国地质大学(北京)地球物理与信息技术学院 
zoucc@cugb.edu.cn 
彭诚 中国地质大学(北京)地下信息探测技术与仪器教育部重点实验室
中国地质大学(北京)地球物理与信息技术学院 
 
杨玉卿 中海油田服务股份有限公司油田技术事业部  
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摘要:
A Study on the Sedimentation Rate of the Denglouku Formation from CCSD SK-2, Based on Logging Spectral Analysis
      The SK-2 of China Continental Scientific Drilling Project (CCSD) in the Songliao Basin recorded the Cretaceous continental sedimentary data. The continuous, multi-parameter, high-resolution geophysical logging data provided an opportunity to study the variation in sedimentation rate in the Songliao Basin. In this study, we used GR, Th, K, and Th/K logging data to calculate the sedimentation rate using the astronomical cycle method and discussed the main controlling factors affecting sediment formation. Spectral analysis results of various logging data showed that the Denglouku Formation has recorded the information of the great Milankovitch cycle information, and the sedimentation process is affected by the driving force of the astronomical orbit. Th data are highly sensitive to astronomical period information, and comprehensively considering the results of various logging data, a continuous and relatively accurate sedimentation rate has been obtained. The sedimentation rate showed a trend from high to low with depth from bottom to top. Sedimentation of the second to third members of the Denglouku Formation was mainly controlled by the faulting activities of the basin, and the overall sedimentation rate was high, reaching a maximum of 16.2 cm/ka. From then on to the fourth member of the Denglouku Formation, the basin transformed into a regional depression structure owing to the gradual weakening of the rifting activity, and the formation had a low sedimentation rate; the lowest rate was 5.9 cm/ka. This study established a continuous sedimentation rate profile of the Denglouku Formation from CCSD SK-2, which provided logging evidence for revealing the geological law of the transition from rifting activity to depression activity in the Songliao Basin.
ZHANG Hao-dong,ZOU Chang-chun,PENG Cheng,YANG Yu-qing.2022.A Study on the Sedimentation Rate of the Denglouku Formation from CCSD SK-2, Based on Logging Spectral Analysis[J].Acta Geoscientica Sinica,43(5):654-664.
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