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The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: The Antarctic Continental Margin
By
Antarctica will surely be the last continent in the world to
be exploited for its oil and gas, if indeed these resources are
ever exploited. Yet, the knowledge we gain from geologic
research on the continent and in the seas that surround it will
help us reconstruct ancient plate configurations, sea levels,
and paleo-oceanographic and paleoclimatic conditions.
Furthermore, ongoing studies of marine sedimentary
processes that occur on the continental margin of Antarctica
can be used to interpret ancient glacial marine sequences,
which are widespread in time and space.
The continent is almost entirely (97%) covered by its ice
sheet, which is thousands of meters thick. Drainage from the
continent is not too unlike that of other continents, except ice
streams, rather than rivers, are the recipients of most of this
drainage. As these ice streams approach the sea they
converge to form large ice shelves and ice tongues. The
ultimate repository for sediments stripped from the continent
are the seas surrounding it, particularly those continental
shelves which bound large ice shelves and ice tongues. Most
of this sediment is transported to large depocenters, which,
like fluvial deltas, are characterized by extensive and thick
prograding sequences. However, sands are rather rare
components of these sequences. Along those portions of the
continental shelf where glacial drainage is limited, the supply
of terrigenous sediment to the sea floor is very slow, and, in
fact, glaciers typically have eroded more sediment than they
have deposited.
Sedimentation on the Antarctic continental margin also is
unique compared to other continental margins of the world.
The continental shelf averages 400 meters in depth, has
extremely rugged glacial topography, and typically slopes
toward the continent. Consequently, waves and wind driven
currents play only a minor role as sedimentary agents, and it is
the impinging deep sea currents and sediment gravity flows
which are the primary agents controlling the distribution of
sand. Turbidites are common on both the shelf as well as the
deep sea floor and several large submarine fans occur around
the continent. The largest of these is the Weddell Abyssal Fan,
which is probably in excess of a million square kilometers. Just
how these fans are supplied with sediment, given the present
great depth of the shelf, is one of our most intriguing, but as yet
unsolved, questions. End_of_Record - Last_Page 2---------------