Clay Sedimentology

ISBN 13: 9783540508892
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Clay Sedimentology by Herve Chamley

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Sedimentology - 1 - Quick overview of clastic sediments - Geology concepts

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Origin, weathering, and geochemical composition of loess in southwestern Hungary. The upper two tills are finer than the lowest two, and the lowest three tills contain more gravel than the upper till. Geochemistry International 45, — Cenozoic continental climatic evolution of Central Europe. No Jacket.

My master thesis was an interdisciplinary subject including sedimentology of carbonates and clay- mineralogy with regard to the Stassfurt Carbonate of the Permian Zechstein in the area of Mecklenburg - Western Pomerania. I especially investigated clay mineral composition and diagenetic processes and compared different facies of the northern Ca2 platform.

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The architecture of the drift deposits is controlled by the interaction of ocean currents whose strengths and boundaries are forced by variations in climate and sea level in addition to local factors such as sediment supply and bottom topography. The relative impacts of these forces on depositional geometries will be assessed.

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Clay Sedimentology is a comprehensive textbook divided into six parts: clay minerals and weathering - clay sedimentation on land - origin and behaviour of. Clay sedimentology. Front Cover. Hervé Chamley. Springer-Verlag, - Science - pages Clay Minerals. 3. Clay Formation through Weathering. 21 .

Why study submarine canyons? There is a general lack of understanding as how these canyons are major player shaping continental margin and guiding sediments from the shallow to deep water marine systems.

Decoding the interaction between contour currents and canyon deposition requires more integrated research if canyon floor sediments are to be used as a paleoceanographic archive. As a main part of this study, I am evaluating the sediments delivered to Mar del Plata Canyon off Argentina during the last 20 ka.

Since the canyon head is situated at a mid-slope position, it is well suited to study all intermediate and deep water masses shaping the continental slope off Argentina.