Guevara, Edgar1, Andres Aslan2, W. A. White1, J. A.
Raney1, J. C. Gibeaut1
(1) University of Texas at Austin, Austin, TX
(2) Mesa State College, Grand Junction, CO
ABSTRACT: The Orinoco Delta, Venezuela: Sedimentation Near an Active Plate Margin
The Orinoco Delta encompasses more than 22,000 km2 of nearly pristine coastal and
deltaic environments near the South America-Caribbean plate margin. Fluvial and marine
interactions and tectonic processes are reflected in the facies character, distribution,
and architecture of this poorly known delta system. Two distinct sectors with contrasting
geomorphic characteristics, sedimentary processes, and lithofacies are recognized.
The southeastern delta plain is dominated by the straight to anastomosing, main
distributary channel (Rio Grande), overbank flooding, and siliciclastic sedimentation. The
coastline is dominated by estuaries, interchannel mangrove islands, and tidal sand ridges.
An intricate network of distributary channels and tidal creeks is present in the northwest
delta plain. Distributary channels produce mud- and peat-encased sand bodies that are up
to 1 km wide and up to 15 m thick. Distributaries separate densely vegetated flood basins
that contain peat up to 10 m thick and, which cover areas as large as 200 km2.
Shoreline progradation in the northwest delta results from progradation of coast-parallel
mudcapes that is triggered by distributary avulsion. The mudcapes, comparable to those of
the Suriname coast, are present along ~100 km of the coast and are comprised of
wave-modified suspended sediment that is largely transported by northwest-directed
longshore currents. Mudcapes are typically 5 to 10 km wide and up to 30 km long.
Transpression along the South American-Caribbean plate margin triggers shale diapirism
manifested by mud volcanoes along the NW coast of the delta. The shale diapirs locally
form hydrocarbon traps.
AAPG Search and Discovery Article #90026©2004 AAPG Annual Meeting, Dallas, Texas, April 18-21, 2004.