LOCK, BRIAN E., University of Southwestern Louisiana, Lafayette, LA
Abstract: Sedimentological Features Within the Edwards Group of West-Central Texas
Shoaling-upward cycles seen in the vicinity of Kerrville and Junction include subtidal, highly burrowed facies passing up into higher energy intertidal grainstones capped by supratidal, commonly stratiform dolomite with gypsum nodule molds, local dedolomite and erosional truncation. These cycles are typically m-scale, and the dolomites can reasonably be interpreted as products of penecontemporaneous sabkha processes.
Further west, near Sheffield, shoaling-upward cycles are an order of magnitude thicker, with oyster wackestones coarsening upwards to gastropod grainstones. Cycle boundaries are abrupt, but not necessarily erosional.
Other types of stratigraphic breaks (diastems) are more subtle, occurring without obvious cyclicity. Hardgrounds -- with (a) oysters cemented on them, (b) blackened surfaces, (c) borings, and (d) overlain by rounded clasts -- indicate submarine exposure, while other, hummocky erosion surfaces are interpreted as karst, resulting from subaerial exposure.
In addition to the stratiform dolomite associated
with the supratidal (sabkha) surfaces described above, lenses of dolomite
seen in the road-cuts near Sonora are interpreted to be related to shallow
subsurface hydrologic pathways, consistent with seepage-reflux models for
dolomitization.
See page 1357 of PDF for this abstract.
AAPG Search and Discovery Article #90924©1999 GCAGS Annual Meeting Lafayette, Louisiana