Abstract
A mathematical model is given for the concentration profile as a function of time, including a T-dependent partitioning of the solute between the two phases. It is illustrated by the partitioning of zirconia between ilmenite and ulvospinel. The cooling rates of a suite of Apollo 15 Elbow Crater gabbros are calculated and the implications are discussed. -K.A.R.
Original language | English (US) |
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Pages (from-to) | 9511-9518 |
Number of pages | 8 |
Journal | Journal of geophysical research |
Volume | 86 |
Issue number | B10 |
DOIs | |
State | Published - 1981 |
ASJC Scopus subject areas
- Geophysics
- Forestry
- Oceanography
- Aquatic Science
- Ecology
- Water Science and Technology
- Soil Science
- Geochemistry and Petrology
- Earth-Surface Processes
- Atmospheric Science
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science
- Palaeontology