Evidence of shock-compressed stishovite above 300 GPa

SiO(2) is one of the most fundamental constituents in planetary bodies, being an essential building block of major mineral phases in the crust and mantle of terrestrial planets (1–10 M(E)). Silica at depths greater than 300 km may be present in the form of the rutile-type, high pressure polymorph st...

Descripción completa

Detalles Bibliográficos
Autores principales: Schoelmerich, Markus O., Tschentscher, Thomas, Bhat, Shrikant, Bolme, Cindy A., Cunningham, Eric, Farla, Robert, Galtier, Eric, Gleason, Arianna E., Harmand, Marion, Inubushi, Yuichi, Katagiri, Kento, Miyanishi, Kohei, Nagler, Bob, Ozaki, Norimasa, Preston, Thomas R., Redmer, Ronald, Smith, Ray F., Tobase, Tsubasa, Togashi, Tadashi, Tracy, Sally J., Umeda, Yuhei, Wollenweber, Lennart, Yabuuchi, Toshinori, Zastrau, Ulf, Appel, Karen
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7311448/
https://www.ncbi.nlm.nih.gov/pubmed/32576908
http://dx.doi.org/10.1038/s41598-020-66340-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7311448/
https://www.ncbi.nlm.nih.gov/pubmed/32576908
http://dx.doi.org/10.1038/s41598-020-66340-y

Ejemplares similares