1887

Abstract

Reported here are some initial results of a computational effort to conduct finite<br>element modelling of the formation of mineral deposits. This includes the<br>convection in a freezing magma chamber and attending hydrothermal circulation<br>in surrounding country rock. Although 2-D calculations will be presented for<br>comparison, we have performed the first 3-D calculations of magma chamber<br>cooling and the response of the surrounding country rock.

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/content/papers/10.3997/2214-4609-pdb.223.020
1997-09-29
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.223.020
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