Basin Analysis in Petroleum Exploration 1994
DOI: 10.1007/978-94-011-0954-3_12
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History of Oil and Natural Gas Production in the Békés Basin

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Cited by 5 publications
(3 citation statements)
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“…The lower measuring limit of the standard laboratory permeability meter was −1 log mD in the 1980s-1990s [10]. One part of the measured samples originates from the fractured part of the formation [60], so the measured higher permeability values do not deliver information about matrix permeability. Two conceptual groups have been formed relating to the overpressure generation mechanisms in case of the Pannonian Basin.…”
Section: Discussionmentioning
confidence: 98%
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“…The lower measuring limit of the standard laboratory permeability meter was −1 log mD in the 1980s-1990s [10]. One part of the measured samples originates from the fractured part of the formation [60], so the measured higher permeability values do not deliver information about matrix permeability. Two conceptual groups have been formed relating to the overpressure generation mechanisms in case of the Pannonian Basin.…”
Section: Discussionmentioning
confidence: 98%
“…A porosity and a permeability measurement program have been carried out in case of underrepresented lithostratigraphic units. Shale-rich formations (delta slope, prodelta, and pelagic sediments) were underrepresented, due to its low hydrocarbon reservoir perspectives [59,60]. The measure program delivered that the finalized porosity-depth and porosity-effective stress trends rely on measured core-based and calculated well logderived porosity values.…”
Section: Porosity Permeability and Compaction Trendsmentioning
confidence: 99%
“…For the Data Collection segment of our study, we utilized data from 67 wells in the study area which is located in the Southern Part of the Bekes Basin, Hungary, a site previously explored for hydrocarbon but now considered for its geothermal potential [29]. This field encompasses two potential formations, the shallow Szolnok Formation as an aquifer [30] and the deeper Bekes Formation [29], offering a unique lens to examine heat storage capabilities. The selection of 3.88 km as the side length for our analysis squares derives from the optimal area typically utilized for injection and production processes within such formations.…”
Section: Data Collectionmentioning
confidence: 99%