Fault-fracture mesh petroleum plays in the Zhanhua Depression, Bohai Bay Basin: Part 2. Oil-source correlation and secondary migration mechanisms

• Published in: Organic geochemistry Vol. 36; no. 2; pp. 203 - 223
• Main Authors: Shi, Dishi, Li, Maowen, Pang, Xiongqi, Chen, Dongxia, Zhang, Shanwen, Wang, Yongshi, Jin, Qiang
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01.02.2005; Elsevier Science
• Subjects: Earth sciences; Earth, ocean, space; Exact sciences and technology; Geochemistry; Marine; Northwest Pacific; Bohai Bay; Yellow Sea; basement; Paleogene; Neogene; depositional environment; reservoirs; upper Tertiary; biodegradation; faults; secondary migration; depressions; Oligocene; brackish water; Cenozoic; fractures; clastic rocks; oil shale; mudstone; crude oil; thermal maturity; hydrocarbons; maturity; Tertiary; biomarkers; source rocks; Eocene; chemically precipitated rocks; carbonates; evaporites; Paleozoic; sedimentary rocks; correlation; Pacific Ocean; Phanerozoic; chemical composition
• ISSN: 0146-6380; 1873-5290
• DOI: 10.1016/j.orggeochem.2004.09.003

The chemical compositions of crude oils from over 20 oilfields in the Zhanhua Depression, Bohai Bay Basin, were studied in order to understand their genetic relationships, thermal maturity and biodegradation ranking. Molecular geochemical parameters indicate the presence of three possible oil families in reservoirs ranging from Paleozoic (basement) to Neogene. A number of biomarker features support deposition of the source rocks for these oils under a wide range of depositional environments. The majority of the oils discovered in the depression belong to the FL family, and display characteristics consistent with a dominantly freshwater (to slightly brackish water) lacustrine source rock in the Es 3 member of the Shahejie Formation. The somewhat geographically restricted SL family oils are apparently linked to saline lacustrine, carbonate-evaporite source rocks distributed mostly in the upper Es 4 member of the Shahejie Formation from the Bonan-Gubei sag areas. The thermally less mature BL family oils occur mostly within the Es 1, Es 2 or Dongying Formation reservoirs near the central sag areas, and show close affinities to the interbedded or intercalating Es 1 calcareous mudstones and oil shales deposited in a slightly saline to dominantly brackish water lacustrine setting. The SL and FL family oils are generally mature, whereas most of the BL family oils usually show low maturity. Oil-source correlation demonstrates strong genetic relationships between the mature Es 4 and Es 3 source rocks of the Eocene–Oligocene Shahejie formation in the sag areas and the oils accumulated in the shallow Neogene petroleum plays. The geochemical data provide strong support for two sharply contrasting hydrocarbon migration scenarios: (1) short distance lateral migration is dominant in the central sag areas; and (2) the fault-fracture mesh facilitated vertical migration, and coupled with the regional porous Guantao Formation sand sheets, makes the structural, stratigraphic and lithological features over basement high blocks the focal points for petroleum accumulation. Therefore, further exploration in this highly mature petroleum province should focus on heavy oils in the shallow Neogene strata and light oils in the tight sandstones of the deep sag areas.