A. V. Stow and D. J. W. Piper D. A. Stow. Grant Institute of Geology, University of Edinburgh West Mains Road, Edinburgh EH9 3JW, Scotland.

A. Piper. Find this author on Google Scholar. Stow, D. Download (pdf, 6. 9 Mb) Donate Read.

In Stow DAV & Piper DJW (eds) Fine-Grained Sediments: Deep-Water Processes and Facies. Geological Society of London Special Publication 15. Blackwell Scientific Publications, Oxford pp 611–645Google Scholar. 2. Stow DAV (1984) Deep-sea elastics; where are we and where are we going? In: Brenchley PJ (ed) Sedimentology: Recent Developments and Applied Aspects. Geological Society London Special Publication, Blackwell Scientific Publications, Oxford (in press)Google Scholar. 3. Stow DAV, Piper DJW (1984) Fine-grained sediments: Deep-water processes and facies. Geological Society London Special.

Fine-Grained Sediments: Deep-Water Processes and Facies. How we measure 'reads'. Cite this publication. Geological Survey of Canada. Heriot-Watt University. 118+ million publications.

Deep Water Processes and Facies, Special Publications-The Geological Society 15, London, 527-560. According to geochemical studies settling of organic matter is highest in areas where deposition of fine grained sediment takes place. has been cited by the following article: TITLE: Studies on Geochemical and Heavy Mineral Characteristics of Sediments of Gosthani River Estuary. AUTHORS: Fatima Rezaye, Shivanna, M. Jagannadha Rao. KEYWORDS: Geochemical Characteristics, Heavy Mineral, Provenance, Estuary, Gosthani River. The organic carbon is often a good index for deciphering depositional environment.

and D. Piper Atlantic Geoscience Centre Geological Survey of Canada Dartmouth, Nova Scotia Canada

and D. Piper Atlantic Geoscience Centre Geological Survey of Canada Dartmouth, Nova Scotia Canada. 1984 Published for The Geological Society by Blackwell Scientific Publications Oxford London Edinburgh Boston Palo Alto Melbourne.

In Fine-Grained Sediments: Deep-Water Processes and Facies (ed. & Piper, D., pp. .Miocene fluvial facies and vertebrate taphonomy in northern Pakistan

In Fine-Grained Sediments: Deep-Water Processes and Facies (ed. 527–560. London: Geological Society of London. Arthur, M. & Sageman, B. B. 1994. Miocene fluvial facies and vertebrate taphonomy in northern Pakistan. In Recent Developments in Fluvial Sedimentology (ed. Ethridge, F. Flores, R. & Harvey, M. 169–176.

There appears to be a continuum of processes affecting the transport and deposition of fine-grained sediments in the deep sea. This results in a facies continuum within which we can recognize three broadly different facies groups: turbidites, contourites, and tes. Several distinct facies models can be defined for each group on the basis of their chief structural, textural, and compositional attributes.

Special Publication of The Geological Society London, 54, 417-430. eds), Fine-Grained Sediments: Deep-Water Processes and Facies, 343-362. Bath: The Geological Society. Special Publication of The Geological Society London 15. Oxford: Blackwell Scientific Publications.