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Abstract

The Palaeocene Al reservoir is located in blocks 30/7a and 30/13, and contained within a metre-scale thickness sand interpreted as the deposit of a single event: the A1 sand. Reservoir-interval core was taken from seven wells, and was subject to sedimentological, micropermeametry and AMS (anisotropy of magnetic susceptibility) analysis.

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/content/papers/10.3997/2214-4609.201406597
1998-10-03
2021-11-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406597
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