--> ABSTRACT: Sequence-Stratigraphic Relationships and Facies, Architecture of Turonian-Campanian Strata, Kaiparowits Plateau, South-Central Utah, by Keith W. Shanley and Peter J. McCabe; #91022 (1989)
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Sequence-Stratigraphic Relationships and Facies, Architecture of Turonian-Campanian Strata, Kaiparowits Plateau, South-Central Utah

Keith W. Shanley, Peter J. McCabe

Outcrop study of the Straight Cliffs Formation in the Kaiparowits Plateau allows examination of facies tract development within a sequence-stratigraphic framework. This approach provides a new perspective to regional chronostratigraphic and lithostratigraphic relationships of Turonian through Campanian strata. These strata are arranged in geometric patterns that can be related to lowstand, transgressive, and highstand system Previous HittractsNext Hit.

Shoreface deposits of the Tropic Shale and the overlying Tibbet Canyon Member record progradation of highstand and late highstand Previous HitsystemsNext Hit Previous HittractsNext Hit. Coarse, laterally amalgamated fluvial clastics of the Smoky Hollow Member, which sharply overlie the Tibbet Canyon Member, represent an abrupt seaward shift in facies Previous HittractsNext Hit due to increased rates of Previous HitseaNext Hit Previous HitlevelNext Hit fall. The lower portion of the Ferron Sandstone Member of the Mancos Shale to the east is interpreted to be the resulting lowstand system tract.

Renewed relative Previous HitseaNext Hit Previous HitlevelNext Hit rise is recorded within the Smoky Hollow by a vertical change from fluvial and floodplain deposits to tidally influenced sandstones capped by a ravinement surface characterized by a thin pebble lag. These strata and the upper portion of the Ferron Sandstone to the east comprise the transgressive system tract. A thin sharks-tooth lag, 6 m above the ravinement surface in Left Hand Collet Canyon, is thought to mark a condensed section recording maximum rate of deepening. Reduced rates of relative Previous HitseaNext Hit Previous HitlevelNext Hit rise resulted in vertical aggradation of the overlying John Henry Member. Aggradation of fluvial sediments is recorded in the western part of the plateau, whereas vertical aggradation of shoreface sandstones is present along the eastern margin. An upward change from low to high to intermediate ratios of overbank to channel de osits within floodplain strata may mark the transition from Previous HitseaNext Hit Previous HitlevelNext Hit rise to fall. Previous HitSeaNext Hit Previous HitlevelTop lowering during the Campanian resulted in deposition of laterally amalgamated, coarse fluvial sandstones of the Drip Tank Member.

AAPG Search and Discovery Article #91022©1989 AAPG Annual Convention, April 23-26, 1989, San Antonio, Texas.