Titlebook: Generation, Accumulation and Production of Europe’s Hydrocarbons III; Special Publication Anthony M. Spencer Conference proceedings 1993 S

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Proton-containing Acceptor Solvents,itudinal joints, sub parallel to the axial trend, and diagonal joints, oblique to the axial trend, are also present although less abundant. The latter are usually associated with zones of strike-slip deformation. Bedding joints are very rare..The overall characteristics of the analyzed jointing are

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https://doi.org/10.1007/978-1-4614-4388-9nd muds underlain by 123 m of homogeneous, structureless sands. A conventional depositional model suggested that this stratigraphy was the result of turbidite deposition on a retreating submarine fan. A fundamental problem arose in that the sand envelope defined on seismic data suggested a confined

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Joint R&D and Industrial Policy in Japan Thelma oil fields. They lie on the western margin of the South Viking Graben and are combined structural/stratigraphic traps. The Ryazanian-Late Callovian strata are subdivided into 11 palynologic units, comprising three sequences bounded by major hiatuses. These correspond to major basin-modifying

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Missile Defense and the Asian Cascade,rassic times, the area was split into structural elements by several phases of tectonic movement. In both shallow- and deep-water environments the sedimentary response to tectonic episodes occurred simultaneously, but differed in lithology and intensity, resulting in a highly varied facies developme

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https://doi.org/10.1007/978-981-13-8359-5nics and sedimentation in the area throughout the Mesozoic and Tertiary..The salt accumulated in the northernmost of two Zechstein basins lying north of the east-west trending Variscan mountain front. Salt withdrawal and dissolution during the Triassic and Early/mid-Jurassic led to the formation of