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Geological Journal of China Universities ›› 2023, Vol. 29 ›› Issue (5): 766-775.DOI: 10.16108/j.issn1006-7493.2022030

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Provenance and Sedimentary Facies of the Member 3 of Paleogene Dongying Formation in the Eastern Part of the Liaohe Depression Tidal Area

XIA Changfa1,LIN Chunming1*,ZHANG Xia1,HUANG Shuya1,LI Xulong1,ZHAO Xuepei1,LI Xin1,SONG Fulai1,ZOU Bingfang2,LI Tiejun2#br#   

  1. 1. School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China;
    2. Research Institute of Petroleum Exploration and Development, PetroChina Liaohe Oilfield Company, Panjin 124010, China
  • Online:2023-10-11 Published:2023-10-10

Abstract: The Member 3 of Paleogene Dongying Formation (E2d3) in the eastern part of the Liaohe Depression tidal area is a key target layer for oil and gas exploration. Based on the data of core and logging, the provenance and sedimentary facies of E2d3 in the study area were analyzed by combining clastic components, heavy minerals, sedimentary elements, and core facies with logging. The analysis results show that there are three provenance systems of the E2d3 in the tidal area, namely northern provenance, eastern provenance, and Yuedong buried hill in the northwest; the sedimentary facies in the study area are mainly composed of the braided river delta frontal subfacies and shore-shallow lacustrine subfacies, which are controlled by the tectonic background and provenance, and the sedimentary distribution of the three subsections in the E2d3 of the study area is relatively similar, the braided river delta front is mainly developed in the northern part of the study area, while the braided river delta front and shore-shallow lacustrine beach-bar are developed in the eastern area, and shoreshallow lacustrine beach-bar is developed in the northwest area. Our study provides a sedimentary geological basis for the further exploration and favorable reservoir prediction of the E2d3 in the east of the Liaohe depression tidal area. 

Key words: Liaohe Depression, Eastern tidal area, Dongying Formation, Prov enance, Sedimentary facies

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