A Detailed Look
inside a Complex Channel Belt: Processes, Rates, and Architecture for an
8K-Duration
Holbrook, John1, Whitney Autin2,
Ronald J. Goble3, Tammy M. Rittenour4, Stephen Marshak5
(1) University of Texas at Arlington, Arlington, TX (2) State University of New
York, Brockport, Brockport, NY (3) University of Nebraska, Lincoln, Lincoln, NE
(4) Utah State University, Logan, UT (5) University of Illinois, Urbana,
Urbana, IL
The
Meander amplitude overall is variable,
producing amalgamated and reworked lateral-accretion elements/point bars of 1
km to 19 km with 5-6 km as typical. Channel-fill elements constitute <25% of
the belt deposits. While the more familiar chute and neck cutoff channel fill
process are common, additional process of splay fill, avulsion fill, and
re-occupation fill are also commonly recognized. Splays are common, but
generally small and thin, except where filling tectonic and depositional lows on
the floodplain surface. Overbank fines are generally minimal within the belt,
but thick on the belt flanks. Belt architecture is hierarchal in the middle 30
km, and includes three subbelts that record tectonically initiated in-belt
avulsion not observed elsewhere in the belt. Meander growth rates are
approximately 5m/year, tectonic response rates are on the scale of a few
centauries, tectonic recovery rates are on the scale of one millennium, and
channels require several hundred years to a few millennia to fill depending
upon process.
AAPG Search and Discover Article #90063©2007 AAPG Annual Convention, Long Beach, California