1887

Abstract

Intra-salt carbonate stringers are the Early Cambrian source rocks and reservoir in the South Oman salt basin. Reservoirs are<br>over-pressured and drilled with salt-saturated heavy barite mud. Formation water is ultra-saline (>300kppm), general<br>porosities are low (< 7%) and salt is often found filling part of the pore space. Each reservoir character creates a contrasting<br>scenario for resistivity evaluation.

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/content/papers/10.3997/2214-4609-pdb.151.iptc13332
2009-12-07
2022-05-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.151.iptc13332
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