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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- Reservoir Aspects in Relationship with Sequence Boundaries in Carbonate Platforms
- Springer Berlin Heidelberg