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Rapid crystallization during recycling of basaltic andesite tephra: timescales determined by reheating experiments
Microcrystalline inclusions within microlite-poor matrix are surprisingly common in low intensity eruptions around the world, yet their origin is poorly understood. Inclusions are commonly interpreted as evidence of crystallization along conduit margins. Alternatively, these clasts may be recycled f...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2017
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5389347/ https://www.ncbi.nlm.nih.gov/pubmed/28402339 http://dx.doi.org/10.1038/srep46364 |