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Abstract

Fractured carbonate reservoirs are commonly extremely heterogeneous. This heterogeneity is caused by fracturing at<br>multi scales superimposed on inherent textures from deposition and diagenesis. In addition, there is an<br>interrelationship between diagenesis and fracture formation, e.g. the matrix properties may change due to reactions<br>with fluids provided by the fracture network or fractures are filled with calcite cement.

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/content/papers/10.3997/2214-4609-pdb.151.iptc13915
2009-12-07
2024-04-16
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.151.iptc13915
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