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Titlebook: Hydrocarbon and Petroleum Geology of France; Alain Mascle Book 1994 Springer-Verlag Berlin Heidelberg 1994 Deformation.Jura.Trias.explorat

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Liassic Source Rocks from Three Wells from the Sea of Iroise (French Western Approaches) and Dorset quality, distribution, and maturation history of the potential source rocks, the most widespread and ma­ ture of which are the Liassic black shales. Sections of the­ se shales have been sampled along the classic field expo­ sures of the Dorset coast, and from cuttings in three wells. The Dorset sect
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The Arzacq-Western Pyrenees ECORS Deep Seismic Profilethe thickness of the Mesozoic sedimentary fill (more than 10 km) of the Arzacq basin are detailed. Northward-dip ping reflectors (at 2–3.5 s) beneath the flysch basin of Mauléon are also detected but are still difficult to interpret (basement or Jurassic?).
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A Reinterpretation of the Stress Regime of the Aquitaine Basin, Southwestern France, and Implication orientations also occur. High-grading the data does not improve the resolution..This widespread lack of directional homogeneity, and the frequency with which ovalization was found to be aligned with well deviation, suggest that horizontal stress anisotropy is weakly developed in much of the Aquitai
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Underground Gas Storage Facilities in Franceally safe and reliable (Table 1)..Two examples are discussed: the first one at Cere-la Ronde is sited in an early Lias aquifer reservoir in the Paris basin; the second one at Etrez (Bresse basin) is a cavities storage in a salt layer of Ohgocene age.
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