The origin of the high-K latites from Camp Creek, Arizona: constraints from experiments with variable fO2 and $$a_{{\text{H}}_{\text{2}} {\text{O}}} $$
- 1 August 1986
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 93 (4) , 504-512
- https://doi.org/10.1007/bf00371720
Abstract
No abstract availableKeywords
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