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Abstract
Gulf Coast Association of Geological Societies Transactions
Volume 54 (2004)
EXTENDED ABSTRACT: Sequence Stratigraphy
of Upper Miocene to Pleistocene Sediments of the Central Mississippi Canyon
and Northern Atwater Valley Areas, Northern Gulf of Mexico
Gonzalez, Hector,1,2 Weimer,
Paul,1 and Bouroullec, Renaud1,3
ABSTRACT
Regional
2D seismic and
well data were used to establish the general sequence stratigraphic
and structural framework of the central Mississippi Canyon and northern
Atwater
Valley pro-traction
areas, northern deep Gulf of Mexico. The continental slope consists
of a complex allochthonous salt system including the Rum roho salt system,
two
isolated salt stocks, and the Sigsbee salt nappe. The depositional
setting
is characterized by three deep intra-slope minibasins and one suprasalt
minibasin. The bulk of Oligocene-Pleistocene sediments that filled
these mini-basins
are primarily turbidites (sheet sands, channel-levee complexes, and
overbank deposits) sourced from the Mississippi Delta system.
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