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2 2014

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Stationary reverse temperature modelling and geothermal resources callibration for the Košice Depression (Eastern Slovakia)

Jacko S., Fričovský B., Pachocka K., Vranovska A.

Technika Poszukiwań Geologicznych

2014

R. 53, nr 1

3--25

The south-eastern part of the Košice Depression contains prospective accumulations of geothermal waters having a discharge temperature of 123–129°C at exploration wells. Clastic rocks of the Neogene formation base (Carpathian) and Triassic dolomites of the Čierna hora Mts. Veporic basement form geothermal water aquifers. Using PETREL software for re-evaluation of seismic sounding results and drilled wells data it was possible to make a more accurate determination of the geological boundaries’ spatial positions, and to create a 3D model of the area delimiting four lithologically and stratigraphically different bodies at the most promising locality (i.e. the Ďurkov village area). Heat flowmodelling calculated the geothermal gradient for each aquifer body, e.g. Sarmatian (Gtr »38.1–60.6°C/km), Badenian (Gtr »41–56.1°C/km), Carpathian (Gtr »38.3–51.4°C/km), and Mesozoic (Gtr »22.4–30.6°C/km). Depth temperature distribution fluctuated between 36°C and 138°C on average (from 500 to 3000 m beneath the surface).

W południowo-wschodniej części Depresji Koszyc występują złoża wód geotermalnych o temperaturze na wypływie 123–129°C. Zbiorniki tych wód budują skały klastyczne formacji neogeńskiej (karpatu) oraz dolomity triasowe gór Čiernej hory należące do podłoża weporskiego. Do ponownej oceny wyników badań sejsmicznych oraz badań otworowych wykorzystano oprogramowanie PETREL, co pozwoliło na dokładniejsze przestrzenne określenie granic geologicznych oraz na opracowanie modelu 3D obszaru ograniczonego czterema różnymi pod względem litologicznym i stratygraficznym ośrodkami skalnymi w najbardziej perspektywicznym obszarze miejscowości Ďurkov. W ramach omawianych w artykule prac wykonano modelowanie przepływu ciepła oraz obliczono gradient geotermalny dla każdego ze zbiorników wód, tj.: sarmackiego (Gtr» 38,1–60,6°C/km), badeńskiego (Gtr» 41–56,1°C/km), karpackiego (Gtr» 38,3–51,4°C/km) oraz mezozoicznego (Gtr» 22,4–30,6°C/km). Temperatury na głębokościach od 500 do 3000 m p.p.t. zmieniają się w zakresie od 36 do 138°C.

Tectonic suture of the meliata (Jaklovce) occurences - mezostructural and microstructural research application

Zakrsmidova B., Nemeth Z., Jacko S.

Geology, Geophysics and Environment

2014

Vol. 40, no. 1

147

The study presents new paleopiezometric data of calcite marbles, contributing to a solution of principal geological and tectonic problems of autochthonous vs. allochthonous position of a carbonate succession north of Jaklovce village in the eastern part of the Northern-Gemeric zone. The Triassic-Jurassic sequences in the Kurtova skala hill are since the 1970s linked with the Meliaticum, so-called Jaklovce succession, but direct tectonic and structural evidences of its allochthonous position were not demonstrated as yet. However, due to the corresponding appearance of both, autochthonous and allochthonous carbonates, the boundary between both complexes was not clearly determined, or even both sequences were considered to be in the autochthonous position with primary lithological transitions towards the Permian bedrock. The dymanic recrystallization of the whole volume of allochthonous calcite marbles was shown by our research. The origin of deformation twins was found in nearly each calcite grain (twinning incidence is almost to 100%). The high number of deformation twins per 1 mm of perpendicular diameter of the grain (D = 173.05-646.25) at the very small size of grains (23.7-42.7 µm) resulted from their recrystallization at high differential stresses 6 = 347.49-429.55 MPa. This differs the allochthonous bodies of the Meliaticum from those of autochthonous Permo-Triassic cover of the Northern Gemericum, which does not exhibit deformation twins and ductile overprint. This difference simultaneously indicates that the total plastic recrystallization of allochthonous marbles should have occurred in the conditions of subduction zone, but their post-exhumation transport occurred with kinematics of the superficial nappe and did not cause any whole-volume recrystallization. The exhumed suite (besides carbonates, radiolarites, mafic, and ultramafic rocks) was overprinted by the two principal Alpine deformation phases AD1 and AD3 of tectonic imbrication and horizontal shearing, causing the origin of brittle-ductile and brittle disjunctive structures. Despite the overprint, the primary bedding (gen. So 330/55°) of allochthonous carbonates remained preserved, and contrasts to general NW-SE trending bedding and secondary foliation of autochthnous sequences.