Tectonic and karstic effects on the western Taurus region, southwestern Turkey: Relations to the present temperature gradients and total organic carbon content
Ih. Demirel et Y. Gunay, Tectonic and karstic effects on the western Taurus region, southwestern Turkey: Relations to the present temperature gradients and total organic carbon content, ENERG SOURC, 22(5), 2000, pp. 431-441
The western Taurus region is one of the promising hydrocarbon provinces and
the largest karstic terrain of Turkey. The Mesozoic Beydaglari units depos
ited in the study area are composed mainly of a carbonate succession which
has potential hydrocarbon source rock of various ages. To confirm the tecto
nic and karstic influence on the regional temperature gradient and total or
ganic carbon content, subsurface data obtained from four drillholes, and th
e results of the surface samples and water samples analyses, were used The
low salinity values (less than 2500 mg / liter) of the formation water and
the measured hole temperatures, indicate the presence of the meteoric water
circulation in the geologic section. Since the Late Miocene, intensive tec
tonic deformations and karstification have provided the development of the
aquifer characteristics of the Beydaglari units. Water circulation in the a
quifer system has influenced the total organic carbon content and karstic c
onduits within carbonates.