Abstract
The theory of intracrystalline distribution is outlined and the relationship between macroscopic and site-mixing properties is discussed. An analysis is made of experimental data for the kinetics of Fe2+-Mg order-disorder in pyroxenes and amphiboles; the ordering observed in natural samples is considered in terms of their cooling history. -R.A.H.
Original language | English (US) |
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Pages (from-to) | 58-99 |
Number of pages | 42 |
Journal | Unknown Journal |
State | Published - 1982 |
Externally published | Yes |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences