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Preferred orientation distribution of shock‐induced planar microstructures in quartz and feldspar
Shocked quartz and feldspar grains commonly exhibit planar microstructures, such as planar fractures, planar deformation features, and possibly microtwins, which are considered to have formed by shock metamorphism. Their orientation and frequency are typically reported to be randomly distributed acr...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
John Wiley and Sons Inc.
2020
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7508181/ https://www.ncbi.nlm.nih.gov/pubmed/32999585 http://dx.doi.org/10.1111/maps.13490 |