Published 1982
| Published
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The Influence of Oxygen Fugacity and Cooling Rate on the Crystallization of Ca-Al Inclusions from Allende
- Creators
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Stolper, E.
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Paque, J.
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Rossman, G. R.
Abstract
Although there appears to be general agreement that some coarse-grained Ca-Al-rich inclusions (CAIs) from Allende passed through a molten or partially molten stage in their evolution, there are several competing hypotheses to account for the formation of the liquid phase in CAIs (e.g., 1-4). Studies of the phase equilibria of CAI compositions can help distinguish between these mechanisms for generating liquids in CAIs.
Additional Information
© 1982 Lunar and Planetary Institute.Attached Files
Published - Rossman_1982p772.pdf
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- 44165
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- CaltechAUTHORS:20140306-072714547
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2014-03-06Created from EPrint's datestamp field
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2019-10-03Created from EPrint's last_modified field
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- Division of Geological and Planetary Sciences