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Abstract

Historically the incorporation of faults in the mapping and modeling of complicated geologic structures has presented geophysicists and geologists with severe problems. Horizons were treated as separate surfaces in space, and faults represented as polygons or centre lines.

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/content/papers/10.3997/2214-4609.201409740
1995-05-29
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409740
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