Clastic Hydrocarbon Reservoir Sedimentology pp 573-632 | Cite as
Sandy Coast (Shore) and Neritic Depositional System
Abstract
As we know, the marine environment is quite different from the continent. In addition to physical and chemical conditions, there are great disparities between coastal and submarine deposition conditions and processes. Because submarine environment characteristics are related to seawater depth, the sea area can be divided by seawater depth into four zones, shore (coast), shallow sea, semi-deep sea, and deep sea. The continental shelf (also called shelf), continental slope, continental rise (also called continental apron), and ocean floor (also called abyssal plain) can be divided by the geomorphic features of the continental margin. Shelf break is the turning point (or zone) of the continental shelf and continental slope.
References
- Barwis, J.H, and M.O. Hayes. 1978. Regional patterns of barrier Island and tidal delta deposition applied to hydrocarbon exploration. In Stratigraphic concepts in hydrocarbon exploration.Google Scholar
- Butler, G.P., P.M. Harris, and C.G.S.C. Kendall. 1982. Recent evaporites from the Abu Dhabi coastal flats. In Deposition and diagenetic spectra of evaporites, ed. C.R. Hand-ford, R.G. Loucks, and G.R. Davies, Society of Economic Paleontologists and Mineralogists Core Workshop 3, Calgary, 33–64.Google Scholar
- Clifton, H.E., R.E. Hunter, and R.L. Phillips. 1971. Depositional structures and processes in the non-barred, high-energy nearshore. Journal of Sedimentary Petrology 41: 651–670.Google Scholar
- Einsele, G. 1992. Sedimentary Basins: evolution, facies, and sediment budget. Heidelberg: Springer-Verlag.CrossRefGoogle Scholar
- Falcon, M. 1998. Essentials of physical geology. Boston, New York: Houghton Mifflin Company.Google Scholar
- Fisk, H.N. 1960. Recent Mississippi river sedimentation and peat accumulation. In 4th Congress Pour Iavancement des’ etudes de stratigraphic et de geologic ducarbonifere, Heerlen, Compt Rendu, ed. Ernest Van Aelst.Google Scholar
- Ginsburg, R.N., and L.A. Hardie. 1975. Tidal and storm deposits, northern Andros Island, Bahamas. In Tidal deposits, ed. R.N. Ginsburg, 201–208. Berlin: Springer.CrossRefGoogle Scholar
- Klein, G.V. 1970. Depositional and dispersal dynamics of intertidal sand bars. Joural of Sedimentary Petrology 40: 1095–1127.Google Scholar
- Komar, P.D. 1976. Beach processes and sedimentation. Englewood Cliffs, NJ: Prentice-Hall Inc.Google Scholar
- Kumar, N., and J.E. Sanders. 1974. Characteristics of near-shore storm deposit; examples from modern (sic) and ancient sediments (abstract); In American Association of Petroleum Geologists, Annual Meetings Abstracts, San Antonio, TX, V. L. P55.Google Scholar
- Nelson, C.H., and A. Maldonado. 1988. Factors controlling depositional patterns of Ebro turbidite systems, Mediterranean Sea. The American Association of Petroleum Geologists, 698–716.Google Scholar
- Purser, B.H. 1973. The Persian Gulf: Holocene carbonate sedimentation and diagenesis in a shallow epicontinental sea, 471p. Berlin: Springer.CrossRefGoogle Scholar
- Reineck, H.E., and I.B. Singh 1973. Depositional sedimentary environments with reference to terrigenous elastics, 439p. Berlin: Springer-Verlag.Google Scholar
- Reinecke, H.E., and I.B. Singh. 1979. Depositional sedimentary environments with reference to terrigenous clastics. Changming Chen and Jiliang Li (Trans.). Beijing: Petroleum Industry Press.Google Scholar
- Reinson, G.E. 1984. Barrier island and associated strand plain systems. In Facies models, 2nd edn, ed. R.G. Walker. Geoscience Canada Reprint Ser 1, Geological Society of Canada, 119–140.Google Scholar
- Schwarz, H.U., G. Einsele, and D. Herm. 1975. Quartz-sandy, grazing-contoured stromatolites from coavStal embayments of Mauritania, West Africa. Sedimentology 22: 539–561.CrossRefGoogle Scholar
- Sellwood, B.W. 1986. Shallow marine carbonate environment. In Sedimentary environment and facies, 2nd edn, ed. H.G. Reading, 283–342. Oxford: Blackwell.Google Scholar
- Shepard, F.P., and D.L. Inman. 1950. Nearshore circulation related to bottom topography and wave refraction Trans. American Geophysical Union Publication 31: 163–198.Google Scholar
- Shinn, E.A. 1983. Tidal flat environment. In Carbonate depositional environment, vol. 33, ed. P.A. scholle AAPG, D.G. Bebout, C.H. Moore, 171–210.Google Scholar
- Walker, R.G. 1984. Facies models, 2nd ed. Toronto: Geological Association of Canada Business and Economic Service Ltd.Google Scholar
- Yu, Xinghe, Junmao Zheng, et al. 1997. The establishment of integrated model on structure, deposition and diagenesis. Acta Sedimentologica Sinica 15 (3).Google Scholar