Self-mixing magma in the Ruiz Peak rhyodacite (New Mexico, USA): A mechanism explaining the formation of long period polytypes of mica
Authors:
- I. PignatelliIPI. Pignatelli
- F. FaureFFF. Faure
- R. Mosser-RuckRMR. Mosser-Ruck
Abstract
No abstract availableThis publication has 82 references indexed in Scilit:
- What factors control superficial lava dome explosivity?Scientific Reports, 2015
- Degassing-driven crystallisation in basaltsEarth-Science Reviews, 2013
- Cation-deficient phlogopitic mica exsolution in diopside from garnet peridotite in SuLu, ChinaLithos, 2009
- Magma heating by decompression-driven crystallization beneath andesite volcanoesNature, 2006
- Cristobalite in Volcanic Ash of the Soufriere Hills Volcano, Montserrat, British West IndiesScience, 1999
- Substitution mechanisms and solubility of titanium in phlogopites from rocks of probable mantle originContributions to Mineralogy and Petrology, 1981
- Application of the faulted matrix model to the growth of polytype structures in micaJournal of Crystal Growth, 1981
- Mécanismes de croissance, polytypisme et polymorphisme de la muscovite hydroxylée synthétiqueJournal of Crystal Growth, 1976
- Growth spirals and complex polytypism in micas. I. Polytypic structure generationActa Crystallographica Section A, 1975
- Raman Spectra of α and β CristobaliteThe Journal of Chemical Physics, 1972