1887

Abstract

Summary

The Lubina-Montanazo field is a carbonate reservoir producing from Tertiary clastics and Cretaceous limestones. An outcrop analogue study has been integrated with subsurface data (image logs, well test interpretations, seismic attributes) to characterize the static and dynamic behavior of the fracture network and its interplay with diagenetic facies.

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/content/papers/10.3997/2214-4609.201413529
2015-06-01
2024-04-24
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References

  1. Roca, E.
    [1994] La evolución geodinámica de la Cuenca Catalano-Balear y áreas adyacentes desde el Mesozoico hasta la actualidad. Acta Geológica Hispánica,29, 3–25.
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    [1982] Estudi estructural de les zones de fractura de Garraf i de Vallcarca (Massís de Garraf).Institut d’Estudis Catalans, Barcelona, 96.
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