Abstract
A mathematical study is made of the transition from a one-component kinetic model to a local-equilibrium one in diffusion-limited metasomatism as the rate constants for a reversible reaction increase. The theoretical results are illustrated by computer calculations. (Journal summary)-A.W.H.
Original language | English (US) |
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Pages (from-to) | 127-133; |
Journal | Geochemistry International |
Volume | 24 |
Issue number | 10 |
State | Published - 1987 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Geochemistry and Petrology