Solvus
From Wikipedia, the free encyclopedia
In a physical or geochemical system, a solvus is a line (binary system) or surface (ternary system) on a phase diagram which separates a homogeneous solid solution from a field of several phases which may form by exsolution or incongruent melting.
An example is the formation of perthite when an alkali feldspar is cooled down.
| Please help improve this article or section by expanding it. Further information might be found on the talk page or at requests for expansion. (December 2007) |

