Titlebook: Basin Analysis in Petroleum Exploration; A case study from th Paul G. Teleki,Robert E. Mattick,János Kókai Book 1994 Springer Science+Busin

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https://doi.org/10.1007/978-3-319-52060-5onate rocks beneath basin fill (TD = 5500 m). For these experiments a vertical-component, wall-locking geophone was used. Energy was generated by an explosive source for one near-offset and two far-offset VSP experiments, and by a Vibroseis source for a walk-away VSP experiment. These sets of VSP da

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Legal Issues of Services of General Interestin. A resource appraisal system was designed for play analysis using a reservoir-engineering geologic model and an analytic probabilistic methodology. The system resulted in a package of computer programs, called FASPUM, for play analysis and play aggregation. Resource estimates of crude oil, nonass

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https://doi.org/10.1007/978-3-030-60599-5 tons* of undiscovered oil and 18.05×10. m. of undiscovered natural gas (recoverable). This compares with discovered amounts (through 1985) of 3.81 million metric tons of oil and 25.40×10. m of natural gas. Among the twelve plays assessed, the delta front play has the highest mean potential for oil,

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,Structure of the Békés Basin Inferred from Seismic Reflection, Well and Gravity Data,rassic rocks overlie Cretaceous rocks. Nappes composed of Paleozoic and older rocks overlying Mesozoic rocks have not been reported; the interpretation of seismic data, however, indicates that such nappes could be present..Mesozoic nappes in the basement occur primarily in two parallel, northeast-so

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,Sequence Stratigraphy of the Békés Basin, lobes, indicates that the Neogene post-rift history of the Békés basin reflects one of the last episodes of filling of the much larger Pannonian Basin. It was not until other subbasins to the northwest, north, and northeast became filled by southward-prograding sediment wedges that the major river

ALE

,Lower Pannonian Deltaic-Lacustrine Processes and Sedimentation, Békés Basin,nding basement highs..Abundant sand-rich turbidites derived from advancing deltas form a thick (963 m) prodelta sequence. Subsequences identified within the prodelta strata include, in ascending order, distal lobe, fan, rare channel, and slumped deposits. Successive fan systems, that originated from

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,Stratigraphic Framework and Sandstone Facies Distribution of the Pannonian Sequence in the Békés Bascending order, these formations are (1) the Tótkomlós and Nagyk?rü Formations, a basal clayey marl and marl unit; (2) the Szolnok Formation, a basinal unit consisting of thick amalgamated beds of very fine grained turbidite sandstone and interbedded marl; (3) the Algy? Formation, consisting of prod

ARK

High Resolution Polarity Records and the Stratigraphic and Magnetostratigraphic Correlation of Latens of Pannonian stratigraphie units in the subsurface, and to a new chronostratigraphic framework and model for the manner and timing of accumulation of late Miocene and Pliocene deposits in the Pannonian Basin. The high resolution polarity zonations also provide new information on the detailed char