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Book Chapter

A Mississippi-Sourced, Middle Miocene (M4), Fine-Grained Abyssal Plain Fan Complex, Northeastern Gulf of Mexico

By
Joseph C. DeVay
Joseph C. DeVay
BHP Petroleum, Houston, Texas, U.S.A.
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David Risch
David Risch
BHP Petroleum, Houston, Texas, U.S.A.
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Erik Scott
Erik Scott
BHP Petroleum, Houston, Texas, U.S.A.
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Chris Thomas
Chris Thomas
BHP Petroleum, Houston, Texas, U.S.A.
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Published:
January 01, 2000

Abstract

Seismic facies mapping and seismic stratigraphic analysis in the northeastern Gulf of Mexico indicate the presence of a middle Miocene fan complex, here termed the M4. This fan complex is interpreted to comprise at least two fourth-order sequences deposited during lowstand by the Mississippi River. Each depositional sequence is well organized in sets of laterally continuous and discontinuous/hummocky seismic reflectors that are interpreted to be sheet-sand lobe, nonleveed channel and distributary channel facies. Sea-floor compensation is shown by east–west migration of the M4 sequences. The average depositional rate across the fan complex was about 0.5 m/1000 yr.

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Contents

AAPG Memoir

Fine-Grained Turbidite Systems

Arnold H. Bouma
Arnold H. Bouma
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Charles G. Stone
Charles G. Stone
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American Association of Petroleum Geologists
Volume
72
ISBN electronic:
9781629812625
Publication date:
January 01, 2000

GeoRef

References

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