Search Results - "Fedor, Ferenc"
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Experimental Rock Characterisation of Upper Pannonian Sandstones from Szentes Geothermal Field, Hungary
Published in Energies (Basel) (01-12-2022)“…The Upper Pannonian (UP) sandstone formation has been utilised for thermal water production in Hungary for several decades. Although sustainable utilisation…”
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Assessing the representative elementary volume of rock types by X-ray computed tomography (CT) – a simple approach to demonstrate the heterogeneity of the Boda Claystone Formation in Hungary
Published in Geologos (01-12-2021)“…X-ray computed tomography (CT) can reveal internal, three-dimensional details of objects in a non-destructive way and provide high-resolution, quantitative…”
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Pore characterization, acoustic and permeability measurements on core plug triplets, from the Miocene Tótkomlós (Calcareous Marl) Formation of the Pannonian-basin, Hungary
Published in Geologia Croatica (28-06-2017)“…The Tótkomlós Calcareous Marl (TCM), a Member of the Late Miocene Endrőd Formation was investigated as a potential cap and source rock and also as a local…”
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Semi-analytical approach to the determination of fracture permeability
Published in GEM international journal on geomathematics (01-12-2023)“…Proppant is one of the major elements of a hydraulic fracture process that can influence the productivity of an oil or gas well. The permeability of a propped…”
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Evaluation of 3D small-scale lithological heterogeneities and pore distribution of the Boda Claystone Formation using X-ray computed tomography images (CT)
Published in Geologia Croatica (01-01-2021)“…This study was undertaken to quantify and evaluate the density and porosity characteristics of a Boda Claystone Formation (BCF) core sample using medical CT…”
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Continuous Wavelet Transformation to Quantify small-scale Cycles of Petrophysical Properties; a New Approach Applied in a Potential Disposal Repository of Nuclear Waste, SW Hungary
Published in Geologia Croatica (01-01-2023)“…Continuous Wavelet Transformation (CWT) was applied to study the small-scale repetitive oscillations of porosity distribution patterns in a 5 m silty-claystone…”
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