Stratigraphic architecture and evolution of a deep-water slope channel-levee and overbank apron: The Upper Miocene Upper Mount Messenger Formation, Taranaki Basin

Author:

Rotzien Jonathan R.,Lowe Donald R.,King Peter R.,Browne Greg H.

Funder

National Science Foundation Graduate Research Fellowship Program

Stanford School of Earth Sciences Siemon W. Muller Fellowship

Eric and Sherry Muller

GNS Science

Chevron Grant

A.I. Levorsen Grant

members of the Stanford Project on Deep-water Depositional Systems (SPODDS)

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference103 articles.

1. Lateral accretion packages (LAPs): an important element in deep water sinuous channels;Abreu;Mar. Pet. Geol.,2003

2. Stratal architecture and origin of lateral accretion deposits (LADs) and conterminous inner-bank levee deposits in a base-of-slope sinuous channel, lower Isaac Formation (Neoproterozoic), East-Central British Columbia, Canada;Arnott;Mar. Pet. Geol.,2007

3. Development and seismic geomorphology of a Miocene slope channel megasystem, Taranaki Basin, New Zealand;Baur,2010

4. Deep-water leveed-channel complexes of the Cerro Toro Formation, Upper Cretaceous, southern Chile;Beaubouef;Am. Assoc. Pet. Geol. Bull.,2004

5. High resolution seismic/sequence stratigraphic framework for the evolution of Pleistocene intra slope basins, western Gulf of Mexico: depositional models and reservoir analogs;Beaubouef,2000

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