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Abstract

The studied Eocene carbonate reservoirs of Gulf of Suez area are primarily fractured and characterized with swarms of high angle fractures and fracture corridors. All these fractures are faulting related, sited in a very complicated structure envelop within the Gulf of Suez rift setting.

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/content/papers/10.3997/2214-4609-pdb.287.1187813
2012-03-04
2024-04-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1187813
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