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...type can be formed in deposition marine areas such as shelf sandstone and turbidity sandstone. ...interaction with shale layer in the deep marine. Shape from deposition of turbidity sandstones can be like a lens, duct, or fans.

...nterpreted to represent a deep-marine mass flow [[sandstone]] deposited by turbidity currents. This Heather sand represents a secondary reservoir interval withi ...and Thelma). These proximal fan-apron systems were the source of sand-rich turbidity currents that fed finer grained clastic material into the deeper parts of t

...81>Prior, D. B., B. D. Bornhold, W. J. Wiseman, Jr., and D. R. Lowe, 1987, Turbidity current activity in a British Columbia fjord: Science, vol. 237, p. 1330–

...1995, Modelling the effects of salt-induced topography on deposition from turbidity currents, in C. J. Travis, H. Harrison, M. R. Hudec, B. C. Vendeville, F. J

...es evident in the cores from the field indicate deposition of this body by turbidity currents. Also, the Yowlumne Sandstune body is lens shaped in cross section

...conditions, often by [[suspension]] deposition. Other processes include [[turbidity flow]]s in the lake interior and wave and current reworking along the lake ...zed sand and gravel bodies to sheet-like, thin, graded beds deposited by [[turbidity flow]]s in distal parts of the fan. Vertical sequences through channelized

...m forming thin-bedded [[mudstone]]s, while slumps, [[debris flow]]s, and [[turbidity current]]s form coarse-grained bodies of [[breccia]], [[conglomerate]], and

...fields. Resedimentation processes include sliding, slumping, debris flows, turbidity currents, and creep (from Surlyk et al).<ref name=Surlyk>Surlyk, F., T. Don ...911–937.</ref> Processes tending to redeposit chalk include debris flows, turbidity currents, slumps, and slides ([[:File:M91FG200.JPG|Figure 6]]).<ref name=Ke

...blankets, either deposited from hemipelagic settling or the muddy tails of turbidity flows, can form permeability barriers to vertical flow in these systems (e.

...transport fine sediments far into the lake, also may transport sediment by turbidity current and density underflows to the basin. So, there are many depositiona

...processes operating in deep oceanic environment such as gravity flows and turbidity currents, driven by down-slope movement of sediment under gravity, and ocea

...reted as a submarine, basin-floor fan complexes deposited by debris flows, turbidity currents, slumps, and suspension<ref name=Duttn2005a /><ref name=Handfrd />