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Abstract

North Oman offers a rare opportunity for making outcrop observations of faults developed in<br>formations that are also the producing reservoirs in the sub-surface. It is possible to look in great<br>detail at fault geometries and associated fault damage zones, both in map view and cross sections.<br>From these observations it is possible to establish the geometrical rules that will help to build static<br>models and interpret faults on seismic. It is also possible to illustrate the impact of the simplifications<br>which are inherent to the static modelling process and assess whether they are acceptable or not to<br>define the most suitable modelling strategy.

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/content/papers/10.3997/2214-4609-pdb.248.017
2010-03-07
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.248.017
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