Unreciprocated sedimentation along a mud-dominated continental margin, Gulf of Mexico, U.S.A.: Implications for sequence stratigraphy in muddy settings devoid of depositional sequences

Author:

Madof Andrew S.,Christie-Blick Nicholas,Anders Mark H.,Febo Lawrence A.

Funder

National Science Foundation

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference116 articles.

1. Active fluid flow in the Eugene Island area, offshore Louisiana;Anderson;Lead. Edge,1991

2. Late Quaternary stratigraphic evolution of the northern Gulf of Mexico margin: a synthesis;Anderson,2004

3. Recycling sediments between source and sink during a eustatic cycle: systems of late Quaternary northwestern Gulf of Mexico basin;Anderson;Earth Sci. Rev.,2016

4. Pliocene Discoaster abundance variations, deep sea drilling project site 606: biochronology and paleoenvironmental implications;Backman,1987

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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