Om. Ilkisik et al., GEOELECTROMAGNETIC AND GEOTHERMIC INVESTIGATIONS IN THE IHLARA VALLEYGEOTHERMAL-FIELD, Journal of volcanology and geothermal research, 78(3-4), 1997, pp. 297-308
The Ihlara Valley is situated within a volcanic are that is formed by
the collision of the eastern Mediterranean plate system with the Anato
lian plate. In this study we will present data from a reservoir monito
ring project over the Ihlara-Ziga geothermal field, located 22 km east
of Aksaray, in central Anatolia. Although identified geothermal resou
rces in the Ihlara Valley are modest, substantial undiscovered fields
have been inferred primarily from the volcanic and tectonic setting bu
t also from the high regional heat flow (150-200 mW m(-2)) on the Kirs
ehir Massif. In 1988 and 1990, geoelectromagnetic surveys were underta
ken by MTA-Ankara to confirm the presence of a relatively shallow (app
roximate to 0.5-1 km), hydrothermally caused conductive layer or zone.
CSAMT and Schlumberger resistivity data show good correspondence with
each other, and 2-D geoelectric models are also in harmony with geolo
gic data and gravity anomalies. The depth of the resistive basement, w
hich is interpreted as Paleozoic limestone, is 200-250 m in the wester
n part and increases eastward (approximate to 600-750 m). This may imp
ly N-S-oriented normal faulting within the survey area. The parameters
of the top layer are a resistivity of 25 to 95 ohm m and a thickness
of between 100 and 250 m. The thickness of the conductive tuffs betwee
n the top layer and the basement, whose resistivity is about 4-5 ohm m
, also increases eastward (from 100 to 450 m). The apparent resistivit
y maps for the frequencies between 32 and 2 Hz reveal a localized low
resistivity anomaly to the east of Belisirma. (C) 1997 Elsevier Scienc
e B.V.