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Deep-Water Depositional System

  • Xinghe Yu
  • Shengli Li
  • Shunli Li
Chapter
Part of the Advances in Oil and Gas Exploration & Production book series (AOGEP)

Abstract

As global petroleum exploration constantly goes deeper underground, exploration based on architecture has matured, and all architectures that can be found have been explored in petroliferous basins with relatively high degrees of exploration. Thus, in the future, exploration should focus on looking for lithostratigraphic reservoirs. The presence of a bathymetric or lowstand fan is the main condition for the formation of stratigraphic traps. As a result, studying deep-water depositional systems, particularly deep-water gravity flow depositional systems, is very important. One of the main scientific challenges in the 21st century is understanding resource formation and exploration mechanisms in deep water (sea).

References

  1. Bouma, A.H. 1962. Sedimentology of some flysch deposits, 168p. Amsterdam: Elsevier.Google Scholar
  2. Coleman, J.M. 1976. Deltas: Processes of deposition and models for exploration, 102p. Champaign: Continuing Education Publ Comp., Inc.Google Scholar
  3. Einsele, G. 2000. Sedimentary basins-evolution, facies, and sediment budget, 1–792. Second: Completely Revised and Enlarged Edition Springer-Verlag.CrossRefGoogle Scholar
  4. Faugères, J.-C., E. Gonthier, and D.A.V. Stow. 1984. Contourite drift molded by deep Mediterranean outflow. Geology 12 (5): 296–300.CrossRefGoogle Scholar
  5. Feng, Zengzhao, Yinghua Wang, Huanjie Liu, Qingan Sha, Wang Defa, et al. 1994. Sedimentology in China. Beijing: Petroleum Industry Press.Google Scholar
  6. Galloway, Duncan D., Eric EJ Wolanski, and Brian BA King. (1996). Modeling eddy formations in coastal waters: a comparison between model capabilities. American Society of Civil Engineers.Google Scholar
  7. Gao, Zhenzhong, Shunshe Luo, Youbin He, et al. 1995. Middle Ordovician contourites in western margin of Ordos. Acta Sedimentologica Sinica 13 (4): 16–25.Google Scholar
  8. Gao, Z.Z., and T.Z. Duan. (1990). Sedimentary facies model of Marine facies in south China. Journal of sedimentary journal, (2): 9–21.Google Scholar
  9. George, T.N. (1956). Sedimentary environments of organic reefs. Science Progress (1933-), 44(175): 415–434.Google Scholar
  10. He, Y.B., and S.S Luo. (1997). The recent advances and prospects of the study on deep-water tractive current deposits. Earth science progress, 12(3): 247–252.Google Scholar
  11. Heezen, B.C., D.B. Ericson and M. Ewing. 1954. Further evidence for a turbidity current following the 1929 Grand Banks earthquake. Deep Sea Research 193–202.Google Scholar
  12. Heezen, B.C., M. Tharp, and M. Ewing. (1959). The Floors of the Oceans I. The North Atlantic. Geological Society of America.Google Scholar
  13. Hollister, and M. Walter. (1963). The mission for a manned expedition to mars. Massachusetts Institute of Technology, 17(6): 759–65.Google Scholar
  14. Klein, G.V. 1977. Tidal circulation model for deposition of clastic sediments in epeiric and mioclinal shelf sea. Sedimentary Geology 18: 1–12.CrossRefGoogle Scholar
  15. Kolla, V., and F. Coumes. (1987). Morphology, internal structure, seismic stratigraphy, and sedimentation of indus fan. AAPG Bulletin, 71(6): 650–677.Google Scholar
  16. Kruit, Cornelis. (1955). Sediments of the Rhone delta: grain size and microfauna. (Doctoral dissertation).Google Scholar
  17. Kuenen, P.H., and C.I. Migiorini. 1950. Turbidity currents as a cause of graded bedding. Journal Geology 58: 41–127.Google Scholar
  18. Kuvaas, B., and G. Leitchenkov. (1992). Glaciomarine turbidite and current controlled deposits in prydz bay, antarctica. Marine Geology, 108(3–4): 365–381.Google Scholar
  19. Larter, R.D., and A.P. Cunningham. (1993). The depositional pattern and distribution of glacial-interglacial sequences on the antarctic peninsula pacific margin. mar geol. Marine Geology, 109(3–4), 203–219.Google Scholar
  20. Locker, S.D., and E.P. Laine. (1992). Paleogene-neogene depositional history of the middle u.s. atlantic continental rise: mixed turbidite and contourite depositional systems. Marine Geology, 103(1–3): 137–164.Google Scholar
  21. Lowe, D.R. (1982). Sediment gravity flows: ii. depositional models with special reference to the deposits of high-density turbidity currents. Journal of Sedimentary Research, 52(6): 343–61.Google Scholar
  22. Liu, Baojun, and Yunfu Zeng, as chief editor. 1985. Lithofacies paleogeography basis and working method. Beijing: Geological Publishing House.Google Scholar
  23. Middleton, G.V. (1973). Sediment gravity flows:mechanics of flow and deposition. Turbidites and deep-water sedimentation, 1–38.Google Scholar
  24. Middleton, G.V., and M.A. Hampton. 1976. Subaqueous sediment transport and deposition by sediment gravity flows. In Marine sediment transport and environmental management, ed. D.J. Stanley, and D.J.P. Swift, 197–218. New York: Wiley.Google Scholar
  25. Mutti, E. (1977). Distinctive thin‐bedded turbidite facies and related depositional environments in the eocene hecho group (south-central pyrenees, spain). Sedimentology, 24(1): 107–131.Google Scholar
  26. Mutti, E. 1985. Turbidite systems and their relations (sic) to depositional sequences, 65–93. In Provenance of arenites, ed. G.G. Zuffa, 379p. Boston: D. Reidel Publishing company.Google Scholar
  27. Mutti, E., and F.R. Lucchi. 1972. Le torbiditi dell Appennino settrentrionale: introduzione all analysis di facies. Società Geologica Italiana, Mem. 11: 161–199.Google Scholar
  28. Normark, W.R. (1970). Channel piracy on monterey deep-sea fan. Deep Sea Research & Oceanographic Abstracts, 17(5): 837–846.Google Scholar
  29. Pudsey, C.J., and J.A. Howe. (1998). Quaternary history of the antarctic circumpolar current: evidence from the scotia sea. Marine Geology, 148(1–2): 83–112.Google Scholar
  30. Reading, H.G., and M. Richards. 1994. Turbidite systems in deep-water basin margins classified by grain size and feeder system. The American Association of Petroleum Geologists 792–821.Google Scholar
  31. Shanmugam, G. 2003. Deep-marine tidal bottom currents and their reworked sands in modern and ancient submarine canyons. Marine and Petroleum Geology 20: 471–491.CrossRefGoogle Scholar
  32. Shanmugam, G. and R.J. Moiola. (1985). Submarine fan models: Problems and solutions. In Submarine fans and related turbidite systems, eds. A.H. Bouma, et al., 29–34. New York: Springer Verlag.Google Scholar
  33. Shanmugam, T.D. Spalding, and D.H. Rofheart. (1995). Deep-marine bottom-current reworked sand (Pliocene-Pleistocene) Ewing Bank 826 Field, Gulf of Mexico. Turbidites and associted deep-water facies, 25–54.Google Scholar
  34. Stow, D.A.V., and M. Mayall. (2000). Deep-water sedimentary systems: new models for the 21st century. Marine & Petroleum Geology, 17(2): 125–135.Google Scholar
  35. Stow, D.A.V., J.C. Faugeres, J.A. Howe, et al. 2002. Bottom currents, contourites and deep-sea sediment drifts; current state-of-the-art. In Deep-water contourite systems: Modern drifts and ancient Selres, seismic and sedimentary characteristics, ed. D.A.V. Stow, C.J. Pudsey, J.A. Howe et al. Vol. 22, 7–20. Geological Society, London, Memoirs.Google Scholar
  36. Tarbuck, and J. Edward. (1984). The earth. C.E. Merrill Pub. Co.Google Scholar
  37. Walker, R.G. 1978. Deep-water sandstone facies and ancient submarine fans: Models for exploration for stratigraphic traps. AAPG 62: 932–966.Google Scholar
  38. Walker, and L. Cherry. (1992). The volcanic history and geochemical evolution of the Hveragerði Region, S. W. Iceland. (Doctoral dissertation, Durham University).Google Scholar
  39. Walker, R.G. (1966). Shale grit and grindslow shales: transition from turbidite to shallow water sediments in the upper carboniferous of northern england. Journal of Sedimentary Research, 36(1): 90–114.Google Scholar

Copyright information

© Springer International Publishing AG, part of Springer Nature 2018

Authors and Affiliations

  1. 1.China University of GeosciencesBeijingChina
  2. 2.China University of GeosciencesBeijingChina

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