Differential hydrocarbon enrichment in deep Paleogene tight sandstones of the Dongpu Depression in Eastern China. Issue 3 (May 2021)

• Record Type: Journal Article
• Authors: Zhang, Yuanyuan; Ren, Zhanli; Jiang, Youlu; Liu, Jingdong
• Is Part Of: Energy exploration & exploitation. Volume 39:Issue 3(2021)
• Page Start: 797
• Page End: 814
• Publication Date: 2021-05
• Subjects: Differential enrichment -- hydrocarbon property -- tight sandstone reservoir -- deep Paleogene -- Dongpu Depression -- Eastern China -- rifted-basin; Power resources -- Periodicals; 333.79
• DOI: 10.1177/0144598720988112
• Languages: English
• ISSNs: 0144-5987

Abstract

To clarify the characteristics and enrichment rules of Paleogene tight sandstone reservoirs inside the rifted-basin of Eastern China, the third member of Shahejie Formation (abbreviated as Es3) in Wendong area of Dongpu Depression is selected as the research object. It not only clarified the geochemical characteristics of oil and natural gas in the Es3 of Wendong area through testing and analysis of crude oil biomarkers, natural gas components and carbon isotopes, etc.; but also compared and explained the types and geneses of oil and gas reservoirs in slope zone and sub-sag zone by matching relationship between the porosity evolution of tight reservoirs and the charging process of hydrocarbons. Significant differences have been found between the properties and the enrichment rules of hydrocarbon reservoirs in different structural areas in Wendong area. The study shows that the Paleogene hydrocarbon resources are quasi-continuous distribution in Wendong area. The late kerogen pyrolysis gas, light crude oil, medium crude oil, oil-cracked gas and the early kerogen pyrolysis gas are distributed in a semicircle successively, from the center of sub-sag zone to the uplift belt, that is the result of two discontinuous hydrocarbon charging. Among them, the slope zone is dominated by early conventional filling of oil-gas mixture (at the late deposition period of Dongying Formation, about 31–27 Ma ago), while the reservoirs are gradually densified in the late stage without large-scale hydrocarbon charging (since the deposition stage of Minghuazhen Formation, about 6–0 Ma). In contrast, the sub-sag zone is lack of oil reservoirs, but a lot of late kerogen pyrolysis gas reservoirs are enriched, and the reservoir densification and hydrocarbon filling occur in both early and late stages.