1887

Abstract

Geological modelling is frequently carried out in two stages. Initially a layer- and fault-based framework is constructed where the main goal is to represent faithfully the 3D geometry of the real geology, as imaged by seismic data. At this stage close attention is paid to the shape, location and connectivity of fault planes.

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/content/papers/10.3997/2214-4609.201405199
2005-06-13
2020-03-31
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405199
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