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Abstract

Najmah-Sarjelu formations corresponding to the Kimmeridgian-Bajocian stage are established source rocks in the Middle-East. Recent<br>concerted and dedicated exploratory efforts in Kuwait have seen the successful up-grade of these formations in to a potential reservoir<br>rock with the contribution from fracture associated porosity. This paper examines the role of various seismic attributes in the identifi cation<br>of fracture corridors of this play. The data presented here are from the Raudhatain fi eld and North West Raudhatain fi eld areas of<br>North Kuwait.

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/content/papers/10.3997/2214-4609-pdb.147.iptc11437
2007-12-04
2024-04-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.147.iptc11437
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