The Influence of Mass-Transport-Deposit Surface Topography on the Evolution of Turbidite Architecture: The Sierra Contreras, Tres Pasos Formation (Cretaceous), Southern Chile

Journal of Sedimentary Research - Tập 79 Số 5 - Trang 287-301 - 2009
Dominic A. Armitage1, Brian W. Romans2, Jacob A. Covault2, Stephan A. Graham1
1Department of Geological and Environmental Sciences, 450 Serra Mall, Building 320, Stanford, California 94305, U.S.A.;
2Department of Geological and Environmental Sciences, 450 Serra Mall, Building 320, Stanford, California 94305, U.S.A.; present address: Chevron Energy Technology Co., 6001 Bollinger Canyon Road, San Ramon, California 94305 U.S.A.

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Journal of Sedimentary Research

Tập 79 Số 5

287-301

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