Stratal attributes and evolution of asymmetric inner- and outer-bend levee deposits associated with an ancient deep-water channel-levee complex within the Isaac Formation, southern Canada

Author:

Khan Zishann A.,Arnott R.W.C.

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference82 articles.

1. Lateral accretion packages (LAPs); an important reservoir element in deepwater sinuous channels;Abreu;Marine and Petroleum Geology,2003

2. The influence of mass-transport-deposit surface topography on the evolution of turbidite architecture; the Sierra Contreras, Tres Pasos Formation (Cretaceous), southern Chile;Armitage;Journal of Sedimentary Research,2009

3. Stratal architecture and origin of lateral accretion deposits (LADs) and conterminuous inner-bank levee deposits in a base-of-slope sinuous channel, lower Isaac Formation (Neoproterozoic), East-Central British Columbia, Canada;Arnott;Marine and Petroleum Geology,2007

4. Bed forms, primary structures and grain fabric in the presence of suspended sediment rain;Arnott;Journal of Sedimentary Petrology,1989

5. Arnott, R.W.C., Wallace, K., Laurin, L., in press. Stratal architecture and temporal evolution of a passive margin mass transport deposit (MTD), Neoproterozoic Isaac Formation, Cariboo Mountains, British Columbia, Canada. SEPM Special Publication 95.

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