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Titlebook: Geology of Gas and Oil under the Netherlands; Selection of papers H. E. Rondeel,D. A. J. Batjes,W. H. Nieuwenhuijs Book 1996 Kluwer Academ

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https://doi.org/10.1007/978-1-349-21550-8 related to basement faults, which have controlled the relative location of the salt structures, the triggering of salt movement, and the rate of salt movement. Differences in development of salt diapirs coincide with structural units. Dip-slip movement along basement faults enabled the upward flow
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On-line Identification in Closed Looposition within each of the five members of the Main Buntsandstein Formation. This Triassic formation was deposited in a semi-arid continental basin. Sediments reached the P and Q quadrants in braided stream complexes from a hinterland to the southeast. The braided stream complexes were flanked by ae
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https://doi.org/10.1007/978-3-642-86417-9sited in a semi-arid continental setting, and includes dune, interdune, sheetsand and fluvial sandstones. Reduction in reservoir quality is caused primarily by dolomite, halite and anhydrite cementation, with minor authigenic illite and chlorite. Integration of pétrographie and isotopic data has all
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When is a Librarian not a Librarian?ssic Posidonia Shale only oil. However, it is now concluded that both have generated oil and gas, and that an additional possible source rock for oil occurs in the lower part of the Lower Jurassic Aalburg Formation. Geochemical ’fingerprints’ have been established to distinguish the different groups
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Virtual Rehearsal Over Networkslds, with a total Stock Tank Oil Initially In Place (STOIIP) of ca. 210 x 10. m. (1.3 x 10. bbls). Reservoirs comprise continental and shallow marine elastics of Late Jurassic to Early Cretaceous age, deposited in syn-rift and post-rift settings. The West Netherlands Basin was created during Late Ju
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https://doi.org/10.1007/978-94-009-0121-6Borehole; Rotliegend; Sediment; Sedimentation; diagenesis; distribution; exploration; gas; geology; petroleum
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978-94-010-6541-2Kluwer Academic Publishers 1996
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