Source and dispersal of silt on northern Gulf of Mexico continental shelf

Conference · Fri Jan 01 00:00:00 EST 1988

OSTI ID:5924338

Peterson, M; Mazzullo, J

The surficial sediment on the continental shelf of the northern Gulf of Mexico is characterized by abundant silty clay which was deposited during the late Pleistocene lowstand and reworked during and after the Holocene transgression. The purposes of this study were to determine the sources of the silt fraction in this surficial sediment by quartz grain roundness and surface texture analysis, and to determine the effects of modern shelf currents upon the distribution of silt. Areal variations in quartz grain roundness and surface texture define six silt provinces on the northern Gulf of Mexico continental shelf. The Mississippi province is the largest province and stretches from the Chandeleur Islands to Matagorda Bay. It is characterized by a mixture of rounded grains that were derived from the sedimentary rocks of the Gulf coastal plain and the Mid-Continent, and angular, fractured grains that were derived from glacial deposits in the northern United States. A comparison of the areal distribution of these six provinces with the late Pleistocene paleogeography of the continental shelf shows evidence for varying degrees of shore-parallel transport of silt by modern shelf currents.

• OSTI ID: 5924338
• Report Number(s): CONF-880301-
• Resource Relation: Conference: Annual meeting of the American Association of Petroleum Geologists, Houston, TX, USA, 20-23 Mar 1988
• Country of Publication: United States
• Language: English

Related Subjects

02 PETROLEUM
CONTINENTAL SHELF
SITE CHARACTERIZATION
GULF OF MEXICO
SILT
ORIGIN
GEOLOGIC DEPOSITS
GRAIN BOUNDARIES
SEDIMENTARY ROCKS
WATER CURRENTS
ATLANTIC OCEAN
CARIBBEAN SEA
CONTINENTAL MARGIN
CRYSTAL STRUCTURE
CURRENTS
MICROSTRUCTURE
ROCKS
SEAS
SURFACE WATERS
020200* - Petroleum- Reserves
Geology
& Exploration