Contrasting
Upper Devonian Foreslopes of the
Playton, Ted E.1,
Charles Kerans2, Phillip E. Playford3 (1) The Univeristy of Texas at Austin, Austin, TX (2) The University
of Texas at Austin, Austin, TX (3) Geological Survey of Western Australia,
Perth, W.A, Australia
Foreslope deposits that flank
reef-rimmed carbonate platforms are composed of sediment gravity flow
architectural elements that have distinct angles of repose and compositions.
The primary elements observed from these systems include 1.) megabreccias (coarse debris
deposits) from reef collapse, 2.) grain flows and
grainy turbidites (grainstone/
gravel deposits) from platform and slope shedding, and 3.) muddy
turbidites and hemipelagites
(siltstone/wackestone deposits) indicating slope
quiescence. The
Twenty-one measured sections tied to
detailed photomosaics were collected for over 10 km2
and 100-500 meters of seismic-scale middle Frasnian
and Famennian foreslope
strata. Middle Frasnian foreslopes
are dominated by grain flows and grainy turbidites
with few thick megabreccias scattered within the
overall stratigraphy. In contrast, Famennian foreslopes display
cyclic vertical successions consisting of megabreccia,
hemipelagite, and grain flows/grainy turbidites.
These differences in sediment gravity
flow proportions and frequency reflect 2nd-order accommodation changes from Frasnian retrogradation to Famennian progradation. Upright
margins of the Frasnian are inherently more stable
than Famennian margins that prograded
over unstable substrates related to relict backstepping
topography. Thus, reef collapse and megabreccia
generation is a common, high frequency process during Famennian
slope development. Frasnian megabreccias,
however, are not common and represent rare catastrophic events that punctuate
typical sand/gravel shedding onto the slope. These observations offer a linkage
between accommodation, margin geometry, and slope element distribution, which
can aid in the prediction of carbonate foreslope
reservoir quality and architecture in the
AAPG Search and Discover Article #90063©2007 AAPG Annual Convention, Long Beach, California