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)|
|Publication status||Published - Jan 1 1987|
All Science Journal Classification (ASJC) codes
- Geochemistry and Petrology