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Discovery of natural MgSiO(3) tetragonal garnet in a shocked chondritic meteorite
MgSiO(3) tetragonal garnet, which is the last of the missing phases of experimentally predicted high-pressure polymorphs of pyroxene, has been discovered in a shocked meteorite. The garnet is formed from low-Ca pyroxene in the host rock through a solid-state transformation at 17 to 20 GPa and 1900°...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2016
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4820389/ https://www.ncbi.nlm.nih.gov/pubmed/27051873 http://dx.doi.org/10.1126/sciadv.1501725 |