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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Pubblicato in:Sci Rep
Autori principali: 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
Natura: Artigo
Lingua:Inglês
Pubblicazione: Nature Publishing Group UK 2020
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Article
Accesso online: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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