1887

Abstract

Our understanding of the architecture of sedimentary basins is usually substantially more complex than we can use to constrain the framework geometry and properties of in the usual numerical simulators typically used for fluid flow and basin-history simulations. "Up-scaling" methods may allow us to at least partially bridge this gap. The question is: what sorts of rock unit geometries do we need to address?

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/content/papers/10.3997/2214-4609.201409671
1995-05-29
2020-09-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409671
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