Source Rock Potential and Maturation
of Deep Wilcox from
South-Central Texas
Wallace G. Dow, P. K. Mukhopadhyay, T. Jackson
Organic-rich shales (TOC > 0.7%) and coals from the Eocene Wilcox Group
between depths of 5,000 and 24,000 ft from south-central Texas are analyzed to
evaluate organic facies, source rock potential, and maturation
. The lowest and
highest vitrinite reflectance and bottom-hole temperature recorded are 0.4% Ro
and 122°F (68°C) at 5,000 ft (1,750 m) and 4.5% Ro and 460°F (256°C)
at 24,000 ft (8,000 m).
Organic petrography reveals four types of organic facies which corroborates
well-log analysis. Three phases of types IIA and IIB oil-prone kerogens are
present and are related to depositional environment. The change in n-alkane
distribution pattern and the hydrogen index of these sediments are controlled
partly by facies and partly by maturation
. These data suggest variability of
organic facies and establish deltaic coal and deep-sea fan or pro-delta shales
in the lower Wilcox as probable source rocks for liquid hydrocarbons in the
south-central Texas Gulf Coast. Generation and expulsion of crude oil took place
during deposition of overlying middle Miocene reservoir facies.
AAPG Search and Discovery Article #91030©1988 AAPG Annual Convention, Houston, Texas, 20-23 March 1988.