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The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: Exploration History of the South Texas
Lower Cretaceous Carbonate Platform
By
The search for hydrocarbons in reservoirs of the
Lower Cretaceous of south-central Texas has been continuous
for more than 60 years. Accumulations have been
found in significant quantities in only four areas: (1) the
very shallow fault traps high on the San Marcos arch in
Caldwell and Guadalupe Counties, (2) a fault trend
stretching across central Atascosa County, (3) a fault
trend extending from southeastern Atascosa County to
southern Gonzales County, and (4) a narrow, elongate
band extending across the entire area known as the
"Stuart City reef trend."
Reservoirs which contain the hydrocarbons were deposited
in a myriad of environments, all related to a broad
carbonate shelf covered by an extremely shallow sea. The
sea deepened dramatically at the shelf margin parallel
with the reef trend. Dolomites contain the accumulations
in the fault trends, and porosity and permeability are
reasonably good. Few limestones in the reef trend were
extremely porous initially, and late cementation diminished
porosity further.
Oil is the dominant hydrocarbon in the shallow fields,
is less dominant in the other fault trends, and is nonexistent
in the reef reservoirs. Proved ultimate recovery for the
fault trends is about 350 million bbl of oil and 1.5 Tcf of
gas. Reserves for dry gas in the reef-trend reservoirs are
difficult to estimate because of highly variable reservoir
conditions, but should fall between 1 and 1.5 Tcf.
Intensity of exploration decreases from late Early
Cretaceous to older rocks. The Sligo limestone still holds
the promise of success, but lies at considerable depths
over much of the area. Edwards and Glen Rose rocks are
more densely explored, but there are ample opportunities for new plays even in these beds. Geologists who examine
cores and cuttings, determine depositional patterns, understand
modern carbonate sedimentology, and study
patterns of diagenesis will have an advantage in developing new concepts for exploration End_of_Record - Last_Page 2---------------