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...

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Publicado no:Sci Rep
Main Authors: 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: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2020
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Article
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC7311448/
https://ncbi.nlm.nih.gov/pubmed/32576908
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-020-66340-y
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