1887

Abstract

An understanding of fluid flow in the earth’s crust is important in many geological<br>and engineering fields. The flow of groundwater is controlled by a ubiquitous<br>network of fractures that occur in all rocks and at all scales (Main et al., 1990;<br>Carter et al., 1990; Guillespie et al., 1993).

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/content/papers/10.3997/2214-4609-pdb.143.12.2
2001-10-09
2022-12-01
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.143.12.2
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