Abstract
Three types of reservoir associated with diagenetic anomaly structures overlain by three important sequence boundaries age recognized in the Lower Cretaceous car bonate platforms of the Jura and the subalpine chains (Fig. 1; Arnaud-Vanneau et al. 1991). These reservoirs, several meters thick (5 to 15 m), present a conformable stratigraphic habit and are located in the inner platform. Their appearance was due to an aerial exposition, but they developed later during diagenetic evolution.
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References
Arnaud-Vanneau A (1980) Micropaléontologie, paléoécologie et sédimentologie d’une plate-forme carbonatée de la marge passive de la Téthys: l’Urgonien du Vercors septentrional et de la Chartreuse (Alpes occidentales). Géol Alp 1:267 pp
Arnaud-Vanneau A, Arnaud H, Beck Ch, Carrio-Schaffhauser E, Cousin M, Dumont Th (1991) Le concept de stratigraphie séquentielle: applications dans le domaine des plates-formes carbonatées et de leurs marges. CNRS, Ecole Thématique, Grenoble-Chambéry, 36 pp
Moore CH (1989) Carbonate diagenesis and porosity. Elsevier, Amsterdam, 339 pp
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© 1994 Springer-Verlag Berlin Heidelberg
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Arnaud-Vanneau, A., Carrio-Schaffhauser, E. (1994). Reservoir Aspects in Relationship with Sequence Boundaries in Carbonate Platforms. In: Mascle, A. (eds) Hydrocarbon and Petroleum Geology of France. Special Publication of the European Association of Petroleum Geoscientists, vol 4. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-78849-9_22
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DOI: https://doi.org/10.1007/978-3-642-78849-9_22
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