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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...

Deskribapen osoa

Gorde:
Xehetasun bibliografikoak
Argitaratua izan da:Meteorit Planet Sci
Egile Nagusiak: Pittarello, Lidia, Ferrière, Ludovic, Feignon, Jean‐Guillaume, Osinski, Gordon R., Koeberl, Christian
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: John Wiley and Sons Inc. 2020
Gaiak:
Sarrera elektronikoa:https://ncbi.nlm.nih.gov/pmc/articles/PMC7508181/
https://ncbi.nlm.nih.gov/pubmed/32999585
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1111/maps.13490
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