By David Mark Hodgson, Stephen S. Flint
Submarine slopes give you the serious hyperlink among shallow-water and deep-water sedimentary environments. They collect a delicate list of sediment provide, lodging creation/destruction, and tectonic methods in the course of basin filling. there's a complicated stratigraphic reaction to the interaction among parameters that regulate the evolution of submarine slope platforms, e.g. slope gradient, topographic complexity, sediment flux and calibre, base-level swap, tectonic surroundings, and post-depositional sediment remobilization approaches. The elevated figuring out of submarine slope platforms has been pushed in part by means of the invention of enormous hydrocarbon fields in morphologically complicated slope settings, comparable to the Gulf of Mexico and offshore West Africa, and has ended in unique case reports and more suitable universal versions for his or her evolution. This quantity brings jointly study papers from smooth, outcrop and subsurface settings to focus on those contemporary advances in knowing of the stratigraphic evolution of submarine slope systems.Also to be had: restrained Turbidite platforms - ISBN 1862391491 Deep-water Sedimentation within the Alpine Basie of SE France - ISBN 1862391483 Deep-Water Contourite approach: smooth Drifts and historic sequence, Seismic and Sedimentary features - ISBN 1862390924
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Additional info for Submarine slope systems: processes and products
20. Internal architecture of the fill of a mixed erosional/depositional type turbidity current channel exposed at Cerro Mirador (Cerro Mirador measured stratigraphic section, 500 m) (Fig. 19). (a) Detailed measured section from basal portion, and schematic upward-fining and thinning of turbidite channel fill. (b) Top of coarse-grained sandstone bed showing crude diffuse lamination interpreted a s T t traction deposits. (c) Amalgamated sandstone beds such as those in (b) comprise most of the channel-fill.
A complete gradation in bedding styles and degree of internal deformation exists in this lithofacies, which we group together and interpret generically as mass transport complexes. In one end member of such deposits, rotated, intact blocks of strata occurring above listric failure surfaces are interpreted as slide deposits (sensu Martinsen 1989). Contrasting deposits consisting of silty or sandy mud-rich matrix with no discernable internal bedding are interpreted as debris-flow deposits. Amalgamated units of this lithofacies form a significant portion of the total stratigraphic thickness of the Tres Pasos Formation, comprising 50% or more of the middle part of the formation.
1996. Near-surface seismic facies at the Korea Strait shelf margin and trough region. Geo-Marine Letters, 16, 49-56. Deposition and stratigraphic architecture of an outcropping ancient slope system: Tres Pasos Formation, Magallanes Basin, southern Chile M . R . S H U L T Z ~,2, A. D. A. com) 3 Current address: Department of Geosciences, DePauw University, Greencastle, IN 46135, USA Abstract: The Tres Pasts Formation, Magallanes Basin, Chile, represents the deposit of a submarine slope depositional system.
Submarine slope systems: processes and products by David Mark Hodgson, Stephen S. Flint