Deep-Water Processes and Facies Models: Implications for Sandstone Petroleum Reservoirs: 5 (Handbook

Deep-water processes and facies models: implications for sandstone petroleum reservoirs. - (Handbook of petroleum exploration and production; 5). 1.
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Basic civil and mechanical engineering by G Shanmugam Book 1 edition published in in English and held by 4 WorldCat member libraries worldwide.

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The stratigraphy, sedimentology, and tectonics of the Middle Ordovician Sevier shale basin in east Tennessee by G Shanmugam 3 editions published between and in English and held by 4 WorldCat member libraries worldwide. Advanced reservoir characterization for the 21st century: Perkins Research Conference by Bob F. Perkins Research Conference Book 2 editions published in in English and held by 3 WorldCat member libraries worldwide. Slump and debris-flow dominated basin-floor fans in the North Sea: Basic mechanical engineering by G Shanmugam Book 1 edition published in in English and held by 2 WorldCat member libraries worldwide.


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Petrographic study of Simpson group Ordovician sandstone, southern Oklahoma by G Shanmugam 1 edition published in in English and held by 2 WorldCat member libraries worldwide. Basin-floor fans in the North Sea: AAPG Bulletin 79 4 p.

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Shen shui chen ji guo cheng yu xiang mo shi by G Shanmugam Book 1 edition published in in Chinese and held by 1 WorldCat member library worldwide. Chemical weed control in the establishment of the legume cover Mucuna cochinchinensis by G Shanmugam Book 1 edition published in in English and held by 1 WorldCat member library worldwide. Paleoflow directions from ripple-cross lamination, ripple marks on bed surfaces, and sole marks point towards southeast, south, and southwest.

The clastic sediments of the Kamouraska were transported into the deep sea by sediment gravity flows that evolved from hyperconcentrated to concentrated density flows, and then to turbidity currents.


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The depositional environment is interpreted to have been a southwest-trending meandering submarine canyon. The exposed part of the canyon deposits is slightly oblique to the strike of slope. If correct, our interpretation establishes the preservation of continental-slope deposits in more distal deep-water siliciclastic sedimentary rocks of the Taconian orogen in Quebec, which traditionally have been interpreted as submarine-fan and or basin-plain deposits. The orientation of a canyon near parallel-to strike of the slope may have been controlled by syn-depositional growth faults.

The coarsest hyperconcentrated flows, which deposited the conglomerate, were restricted to the deepest parts of the canyon during its early stages of development, whereas the concentrated density flows that deposited the massive quartz-arenite beds covered a wider area. Pierre Malhame , Reinhard Hesse. Canadian Journal of Earth Sciences , , 52 4: Canadian Journal of Earth Sciences. Biostratigraphic significance of lower Paleozoic microfaunas from eastern Canada. Canadian Journal of Earth Sciences 41 5: Morphology and architecture of the present canyon and channel system of the Zaire deep-sea fan.

Marine and Petroleum Geology 19 4: The flow of cohesionless grains in fluids. Diagnostic parameters for comparing modern submarine fans and ancient turbidite systems. In Submarine fans and related turbidite systems. Springer-Verlag, New York, N. Development of large submarine canyons in the Bering Sea, indicated by morphologic, seismic and sedimentologic characteristics. Geological Society of America Bulletin Ordovician and Silurian metamorphic cooling ages along the Laurentian margin of the Quebec Appalachians: Bridging the gap between New England and Newfoundland.

Quantitative analysis of the geometry of submarine channels: Plate tectonics and sandstone compositions. Geological Survey of Canada, Memoir Flow transformations in sediment gravity flows.

Deep water geomorphology of the mixed siliciclastic-carbonate system, Gulf of Papua. Journal of Geophysical Research Morphology of a large meandering submarine canyon system on the Peru—Chile forearc. Marine Geology Canadian Journal of Earth Sciences Ice-sheet sourced juxtaposed turbidite systems in Labrador Sea.

Geoscience Canada 24 1: Loss of capacity, not competence, as the fundamental process governing deposition from turbidity currents. Journal of Sedimentary Research A Depositional mechanics of thick-bedded sandstones at the base of a submarine slope, Tourelle Formation Lower Ordovician , Quebec, Canada.

In Geology of continental slopes. Canadian Journal of Earth Sciences 44 4: Evolution of the Late Cretaceous fore-arc basin of northern and central California. Geological Society of America Bulletin 90 9: New views of granular flows. Geochemical evolution of an Ordovician island arc of the central Newfoundland Appalachians. American Journal of Science 2: Evolution of deep-water Tertiary sinuous channels offshore Angola West Africa and implications for reservoir architecture.

Shanmugam, G. (Ganapathy) 1944-

Origin of the megarhythms in flysch sequences of the Quebec Appalachians. Canadian Journal of Earth Sciences 16 7: In Canadian paleontology and biostratigraphy seminar. Appalachian foreland basins of Canada. In Sedimentary basins of the world Series editor: The sedimentary basins of the USA and Canada.

G. Shanmugam (Author of Deep-Water Processes and Facies Models)

Elsevier Science, Amsterdam, The Netherlands. Stratigraphic framework for the Cambrian—Ordovician rift and passive margin successions from southern Quebec to western Newfoundland. Canadian Journal of Earth Sciences 40 2: Petroleum resource assessment, Paleozoic successions of the St. Lawrence Platform and eastern Appalachians of Canada. Geological Survey of Canada, Open File Can dispersive pressure cause inverse grading in grain flows? Journal of Sedimentary Research 73 2: Journal of Sedimentary Research 72 1: Morphological and seismic characteristics of the Kaoping submarine Canyon.

Marine Geology 1—2: Water escape structures in coarse-grained sediments. Sediment gravity flows II: Depositional models with special reference to the deposits of high-density turbidity currents.


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