Download Submarine slope systems: processes and products by David Mark Hodgson, Stephen S. Flint PDF

By David Mark Hodgson, Stephen S. Flint

Submarine slopes give you the serious hyperlink among shallow-water and deep-water sedimentary environments. They gather a delicate checklist of sediment offer, lodging creation/destruction, and tectonic strategies in the course of basin filling. there's a advanced stratigraphic reaction to the interaction among parameters that regulate the evolution of submarine slope structures, e.g. slope gradient, topographic complexity, sediment flux and calibre, base-level swap, tectonic atmosphere, and post-depositional sediment remobilization procedures. The elevated knowing of submarine slope structures has been pushed in part via the invention of enormous hydrocarbon fields in morphologically complicated slope settings, corresponding to the Gulf of Mexico and offshore West Africa, and has ended in distinctive case stories and greater conventional versions for his or her evolution. This quantity brings jointly examine papers from smooth, outcrop and subsurface settings to focus on those contemporary advances in realizing of the stratigraphic evolution of submarine slope systems.Also on hand: limited Turbidite platforms - ISBN 1862391491 Deep-water Sedimentation within the Alpine Basie of SE France - ISBN 1862391483 Deep-Water Contourite procedure: smooth Drifts and old sequence, Seismic and Sedimentary features - ISBN 1862390924

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ALONSO,B. & BARAZA,J. 1992. Sedimentary evolution of the northwestern Alboran Sea during the Quaternary. Geo-Marine Letters, 12, 144-149. , ALONSO, B. & BARAZA, J. 1994a. PostCalabrian sequence stratigraphy of the northwestern Alboran Sea (southwestern Mediterranean). Marine Geology, 120, 249-265. , ALONSO,B. I. 1994b. Pleistocene progradational growth pattern of the northern Catalonia continental shelf (northwestern Mediterranean). Geo-Marine Letters, 14, 264-271. , GONTHIER, E. V. 1984. Contourite drift molded by deep Mediterranean outflow.

As these channel-fill units are not wholly confined within their erosional containers, and marginal areas appear to interfinger with axial facies, these may be characterized as fills of erosional/depositional type channels (sensu Mutti & Normark 1991). In some cases, silty mudstone drapes (lithofacies 1) overlie such incision features, producing draped scour surfaces that can be continuous for hundreds of metres to kilometres (Fig. 9). Stratigraphic architecture: turbidite channel-fill complexes.

Oxygen isotopes, ice volume and sea level. Quaternary Science Reviews, 6, 183-190. R. & REY, J. 1997. Continental shelf architecture and sealevel cycles: Late Quaternary high-resolution stratigraphy of the Gulf of C~idiz, Spain. Geo-Marine Letters, 17, 133-139. -C. & GONTHIER, E. 1986. Facies distribution and textural variation in Faro Drift contourites: velocity fluctuation and drift growth. Marine Geology, 72, 71-100. R. L. 1985. Late Quaternary shelf-margin deltas, northwest Gulf of Mexico. American Association of Petroleum Geologists Bulletin, 69, 77-91.

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