G
Ganapathy Shanmugam
Researcher at University of Texas at Arlington
Publications - 99
Citations - 6850
Ganapathy Shanmugam is an academic researcher from University of Texas at Arlington. The author has contributed to research in topics: Turbidity current & Sedimentary depositional environment. The author has an hindex of 39, co-authored 94 publications receiving 6140 citations. Previous affiliations of Ganapathy Shanmugam include Mobil & College of William & Mary.
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Significance of Coniferous Rain Forests and Related Organic Matter in Generating Commercial Quantities of Oil, Gippsland Basin, Australia
TL;DR: In the Gippsland basin, coniferous rain forests dominated by kauri vegetation flourished in a raised bog setting as mentioned in this paper, which provided large quantities of hydrogen-rich exinite macerals with potential to generate oil.
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50 years of the turbidite paradigm (1950s—1990s): deep-water processes and facies models—a critical perspective
TL;DR: In this paper, a slope model is proposed that is a debris-flow dominated setting with both non-channelized and channelized systems, based on fluid rheology and flow state.
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Fan-deltas and braid deltas: Varieties of coarse-grained deltas
TL;DR: Fan-delta and braid deltas are two types of coarse-grained deltaic structures that form where an alluvial fan is deposited directly into a standing body of water from an adjacent highland as mentioned in this paper.
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Sequence of structures in fine-grained turbidites: Comparison of recent deep-sea and ancient flysch sediments
TL;DR: A comparative study of the sequence of sedimentary structures in ancient and modern fine-grained turbidites is made in three contrasting areas as discussed by the authors, namely, Holocene and Pleistocene deep-sea muds of the Nova Scotian Slope and Rise, Middle Ordovician Sevier Shale of the Valley and Ridge Province of the Southern Appalachians, and Cambro-Ordovician Halifax Slate of the Meguma Group in Nova Scotia.
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High-density turbidity currents; are they sandy debris flows?
TL;DR: The concept of high-density turbidity current refers to high-concentration, commonly nonturbulent, flows of fluids in which sediment is supported mainly by matrix strength, dispersive pressure, and buoyant lift as mentioned in this paper.