Abstract
The Mississippi Fan consists of 17 discrete channel-levee systems deposited during the late Pliocene and Pleistocene. Each channel-levee system comprises one to several individual channels that vary considerably in distribution, size, and geometry. Their physical characteristics are best described using four parameters—aggradation, lateral migration, sinuosity, and bifurcation. Values for these parameters differ considerably both between and within individual channel-levee systems. Specifically, maximum aggradational values for channels range from 250 to 850 m, whereas lateral migration within the channel valleys range from 0 to 12 km. Channel sinuosities range from none to a moderate amount. Downfan channel bifurcation varies from 0 to 27. The lateral migration of high-amplitude reflections (coarse-grained deposits) within channel valleys is usually associated with sinuous, possibly meandering channels. However, one channel (#13) has 10–12 km of lateral migration and low sinuosity, indicating that lateral migration of submarine fan channels is not always associated with high sinuosity. Channel width/thickness ratios generally decrease downfan, with upfan lateral migration changing downfan to bifurcating channels that show little lateral migration. In many channel-levee systems, the initial channels are relatively small and the levee sediments are possibly slightly coarser-grained; with growth they evolve into wider, larger channels with finger-grained levee sediments.
The depositional variations within the channel valleys are caused by the interplay of several factors. Aggradation reflects the thickness of the coarse-grained channel-fill deposits, and the thickness is partially influenced by the position on the fan surface. Lateral migration was caused probably by deflection of turbidity flows away from previous deposits, as well as downfan avulsion and longevity of channel. Sinuosity is probably controlled by changes in gradients of valley slope and channel slope, and changes in the grain size of the turbidity flows. Bifurcation can be caused by flowstripping, abrupt increases in volume of turbidity flows being delivered to the basin, channel blockage by slides, and levee failure away from the channel. In any channel-levee system, the vertical change in channel deposits and grain size of levees were affected by changes in the grain sizes of flows being delivered to the basin. The initial flows were possibly slightly coarser-grained and became fine-grained during later channel deposition.
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References Cited
Armentrout, J.M., 1987: Testing a benthic foraminiferal biofacies model-PlioPleistocene, Gulf of Mexico: integration of biostratigraphy and seismic stratigraphy: Soc. Econ. Paleont. Mineral.-Gulf Coast Section Eighth Annual Research Conference, p. 6–14.
Bouma, A.H., Stelting, C.E., and Coleman, J.M., 1983/1984: Mississippi Fan: Internal structure and depositional processes; Geo-Marine Lett., v. 3, p. 147–153.
Bouma, A.H., Coleman J.M., and DSDP Leg 96 Shipboard Scientists, 1985: Mississippi Fan: Leg 96 program and principal results, in A.H. Bouma, W.R. Normark, and N.E. Barnes, eds., Submarine fans and related turbidite systems: New York, Springer-Verlag, p. 247–252.
Bouma, A.H., Coleman, J.M., and Meyer, A.W., ed, 1986: Initial reports of the Deep Sea Drilling Project, DSDP Leg 96; U.S. Government Printing Office, Washington, D.C., 824 p.
Bowen, A.J., Normark, W.R., and Piper, D.J.W., 1984: Modelling of turbidity currents on Navy submarine Fan, California Continental Borderland; Sedimentology, v. 30, p. 681–694.
Coleman, J.M., and Roberts, H.H., 1988: Sedimentary development of the Louisiana continental shelf related to sea level cycles; part 2, seismic response; Geo-Marine Lett., v. 8, p. 109–119.
Cremer, M., 1983: Approaches sedimentologiques et geophysiques des accumulations turbiditiques. L’eventail profond du Cap-Ferret, la serie des Gres d’An-not: Ph.D. Thesis; University of Bordeaux I, 334 p.
Cremer, M., Orsolini, P., and Ravenne, C., 1985: Cap-Ferret Fan, Atlantic Ocean, in A.H. Bouma, W.R. Normark, and N.E. Barnes, eds., Submarine fans and related turbidite systems; Springer-Verlag, New York, p. 113–120.
Damuth, J.E., Flood, R.D., Kowsmann, R.O., Belderson, R.H., and Gorini, M.A., 1988: Anatomy and growth pattern of Amazon deep-sea fan as revealed by long-range side-scan sonar (GLORIA) and high resolution seismic studies; Am. Assoc. Petrol. Geol. Bull., v. 72, p. 885–911.
Damuth, J.E., Kolla, V., Flood, R.D., Kowsmann, R.O., Monteiro, M.C., Gorini, M.A., Palma, J.J.C., and Belderson, R.H., 1983: Distributary channel meandering and bifurcation patterns on Amazon deep-sea fan as revealed by long-range sonar (GLORIA); Geology, v. 11, p. 94–98.
Droz, L., and Bellaiche, G., 1985: The Rhone deep-sea fan: morphostructure and growth pattern; Am. Assoc. Petrol. Geol. Bull., v. 69, p. 460–479.
EEZ Scan 84 Scientific Staff, 1986: Atlas of the Exclusive Economic Zone, western coterminous United States; U.S.G.S. Misc. Inves. Series I-1792, 152 p.
EEZ Scan 86 Scientific Staff, 1987: Atlas of the Exclusive Economic Zone, Gulf of Mexico and eastern Caribbean areas; U.S.G.S. Misc. Inves. Series I-1864-a, 104 p.
Feeley, M.H., 1984: Seismic stratigraphie analysis of the Mississippi Fan; unpublished Ph.D. Thesis, Texas A and M, 209 p.
Flood, R.D., and Damuth, J.E., 1987: Quantitative characteristics of sinuous distributary channels on the Amazon deep-sea fan; Geol. Soc. Am. Bull, v. 98, p. 728–738.
Garrison, L.E., Kenyon, N.H., and Bouma, A.H., 1982: Channel systems and lobe construction in the Mississippi Fan; Geo-Marine Lett., v. 2, p. 31–39. Kastens, K.A., and Shor, A.N., 1985: Depositional process of a meandering channel on Mississippi Fan; Am. Assoc. Petrol. Geol. Bull., v. 69, p. 190–202.
Kastens, K.A., and Shor, A.N., 1986: Evolution of a channel meander on the Mississippi Fan; Marine Geol., v. 71, p. 165–175.
Leopold, L.B., and Wolman, M.G., 1960: River meanders: Geol. Soc. Am. Bull.; v. 71, p. 769–794.
Manley, P.L., and Flood, R.D., 1988: Cyclicity in fan development within the upper/middle Amazon Fan; Am. Assoc. Petrol. Geol. Bull., v. 72, p. 912–925.
Mitchum, R.M., Vail, P.R. Vail, and Sangree, J.B., 1977: Seismic stratigraphy and global changes of sea level, Part 6: Stratigraphie interpretation of seismic reflection patterns in depositional sequences, in C.E. Payton, ed., Seismic stratigraphy-applications to hydrocarbon exploration; Am. Assoc. Petrol. Geol. Memoir 26, p. 117–143.
Moore, G.T., Starke, G.W., Bonham, L.C., and Woodbury, H.O., 1978: Mississippi Fan, Gulf of Mexico-physiography, stratigraphy, and sedimentation patterns, in A.H. Bouma, G.T. Moore, and J.M. Coleman, eds., Framework, facies and oil-trapping characteristics of the upper continental margin; Am. Assoc. Petrol. Geol. Studies Geol. No. 7, p. 155–191.
Moore, G.T., Woodbury, H.O., Worzel, J.L., Watkins, J.S., and Starke, G.W., 1979: Investigation of the Mississippi Fan, Gulf of Mexico, in J.S. Watkins, L. Montadert, and P.W. Dickerson, ed, Geological and geophysical investigations of continental margins; Am. Assoc. Petrol. Geol. Memoir 29, p. 383–402.
Mutti, E., 1985: Turbidite systems and their relations to depositional sequences, in G.G. Zuffa, ed.; Provenance of arenites; Reidel, Dordrecht, p. 65–93.
Nelson, C.H., and Maldonado, A., 1988: Factors controlling depositional patterns of Ebro turbidite systems, Mediterranean Sea; Am. Assoc. Petrol. Geol. Bull., v. 72, p. 698–716.
O’Connell, S.B., 1986: Anatomy of modern submarine depositional and distributary systems; unpublished Ph.D. dissertation, Columbia University, New York, 298 p.
Piper, D.J.W., and Normark, W.R., 1983: Turbidite depositional patterns and flow characteristics, Navy Submarine Fan, California Borderland; Sedimentology, v. 30, p. 681–694.
Ramsayer, G.R., 1979: Seismic stratigraphy, a fundamental exploration tool; Offshore Technology Conference Proceedings, v. 3, Paper 3568, p. 1859–1867.
Sangree, J.B., Vail, P.R. Vail, and Sneider, R.M., 1988: Evolution of facies interpretation of the shelf-slope: application of the new eustatic framework to the Gulf of Mexico; Offshore Technology Conference Proceedings 5695, p. 133–144.
Schumm, S.A., 1977: The fluvial system; John Wiley, New York, 338 p. Steffens, G., 1986: Pleistocene entrenched valley/canyon systems, Gulf of Mexico; Am. Assoc. Petrol. Geol. Bull., v. 70, p. 1189 (abstr).
Stelting, C.E., Pickering, K.T., Bouma, A.H., Coleman, J.M., Cremer, M., Droz, L., Meyer-Wright, A.A., Normark, W.R., O’Connell, S., Stow, D.A.V., and DSDP Leg 96 Shipboard Scientists, 1985a: Drilling results on the middle Mississippi Fan, in A.H. Bouma, W.R. Normark, and N.E. Barnes, eds., Submarine fans and turbidite systems; Springer-Verlag, New York, p. 277–282.
Stelting, C.E., and DSDP Leg 96 Shipboard Scientists, 1985b: Migratory characteristics of a mid-fan meander belt, Mississippi Fan, in A.H. Bouma, W.R. Normark, and N.E. Barnes, eds., Submarine fans and turbidite systems; Springer-Verlag, New York, p. 283–290.
Stuart, C.J., and Caughey, C.A., 1976: Form and composition of the Mississippi Fan; Gulf Coast Assoc. Geol. Soc. Trans., v. 26, p. 333–343.
Trainor, D.M., and Williams, D.E., 1987: Isotope chronstratigraphy: High resolution stratigraphie correlations in deep-water exploration tracts of the northern Gulf of Mexico; Gulf Coast Assoc. Geol. Soc. Trans., v. 37, p. 247–254.
Vail, P.R., 1987: Seismic stratigraphy interpretation procedure, in A.W. Bally, ed., Atlas of seismic stratigraphy; Am. Assoc. Petrol. Geol. Studies Geol. No. 27, v. I, p. 1–10.
Vail, P.R., Mitchum, R.M., Todd, R.G., Widmier, J.M., Thompson, S., Sangree, J.B., Bubb, J.N., and Hatelid, W.G., 1977: Seismic stratigraphy and global changes in sea level, Parts 1–11, in C.E. Payton, ed., Seismic stratigraphy-applications to hydrocarbon exploration; Am. Assoc. Petrol. Geol. Memoir 26, p. 51–212.
Walters, R.D., 1985: Seismic stratigraphy and salt tectonics of Plio-Pleistocene deposits, continental slope and upper Mississippi Fan, northern Gulf of Mexico; Unpublished M.A. Thesis, The University of Texas at Austin, 204 p.
Weimer, P., 1989: Sequence stratigraphy of the Mississippi Fan (PlioPleistocene), Gulf of Mexico; Geo-Marine Lett., v. 9, p. 185–272.
Weimer, P., 1990: Sequence stratigraphy, seismic geometries, and depositional history of the Mississippi Fan, deep Gulf of Mexico; Am. Assoc. Petrol. Geol. Bull, v. 74, p. 425–453.
Weimer, P., and Buffler, R.T., 1988: Distribution and seismic facies of the Mississippi Fan channels; Geology, v. 16, p. 900–903.
Weimer, P., and Buffler, R.T., 1989: Seismic definition of fan lobes, Mississippi Fan, Gulf of Mexico; in A.W. Bally, ed., Atlas of seismic stratigraphy: Am. Assoc. Petrol. Geol. Studies Geol. No. 27, v. 3, p. 79–87.
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Weimer, P. (1991). Seismic Facies, Characteristics, and Variations in Channel Evolution, Mississippi Fan (Plio-Pleistocene), Gulf of Mexico. In: Weimer, P., Link, M.H. (eds) Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems. Frontiers in Sedimentary Geology. Springer, New York, NY. https://doi.org/10.1007/978-1-4684-8276-8_18
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DOI: https://doi.org/10.1007/978-1-4684-8276-8_18
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