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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...

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Detalles Bibliográficos
Autores principales: Pittarello, Lidia, Ferrière, Ludovic, Feignon, Jean‐Guillaume, Osinski, Gordon R., Koeberl, Christian
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2020
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