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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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樓主
發(fā)表于 2025-3-21 16:23:16 | 只看該作者 |倒序瀏覽 |閱讀模式
期刊全稱Basin Analysis in Petroleum Exploration
期刊簡稱A case study from th
影響因子2023Paul G. Teleki,Robert E. Mattick,János Kókai
視頻videohttp://file.papertrans.cn/182/181287/181287.mp4
圖書封面Titlebook: Basin Analysis in Petroleum Exploration; A case study from th Paul G. Teleki,Robert E. Mattick,János Kókai Book 1994 Springer Science+Busin
影響因子This volume summarizes in 16 chapters the petroleum geology ofthe Békés basin with respect to its geological settingin the Pannonian Basin. The work was accomplished by a joint effort ofthe Hungarian Oil and Gas Co. and U.S. Geological Survey. .In contrast with other books that discuss the geology of Hungary, thisvolume identifies, in detail, potential source rocks and reservoirrocks, and evaluates the maturation, generation, migration, andentrapment of hydrocarbons. The outstanding points are: (1) itssummary of the petroleum geology of the Békés basin withrespect to its structural and sedimentological setting in thePannonian Basin; (2) the identification of geographic areas,structural trends and stratigraphic zones that remain relativelyunexplored; and (3) a summary of `petroleum plays‘ with an assessmentof their recoverable, undiscovered resources of oil and gas. .This book is primarily for petroleum geologists interested in oil andgas exploration in Hungary, and earth scientists interested in thegeology of the Pannonian Basin. .
Pindex Book 1994
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,Sequence Stratigraphy of the Békés Basin, in late Badenian time (16.5 Ma) when marine waters were shallow (<200 m). By late Sarmatian or early Pannonian time (12?10 Ma), lacustrine conditions prevailed and water depths in the basin increased as a result of basin subsidence rates that greatly exceeded sedimentation rates. The latest history
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Facies and Depositional Environments of Miocene Sedimentary Rocks,ression of the Paratethys Sea is marked by conglomerate and/or breccia that is present almost everywhere where Miocene deposits occur. The Miocene sequence is 0-275 m thick, where penetrated by wells in the Békés basin; however, in the deepest parts of the basin the sequence is inferred to be more t
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,Abnormal Pressure and Hydrocarbon Migration in the Békés Basin,argins of the basin. The producing rocks range in age from Precambrian to Pliocene. Exploration for stratigraphic traps should result in the discovery of many new oil and gas fields. A study of reservoir pressures and migration has been made to help evaluate the hydrocarbon potential of various stra
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