1887

Abstract

The Austrian field Hochleiten at the margin of the Vierma basin is highly compartmentalised, due to intensive faulting. Moreover, the reservoir sands are mainly of deltaic origin and thus often laterally heterogeneous. Because of these discontinuities, a waterflooding program in the field did not work as desired. Seismic and geology give the general framework of the reservoir architecture, but the details of sandbody connections cannot be assessed in this way.

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/content/papers/10.3997/2214-4609.201406360
1999-08-18
2021-03-06
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406360
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