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Subject Item: n2:
rdf:type: n3:
rdfs:label: Stishovite
rdfs:comment: The only known occurrences of stishovite in nature formed at the very high shock pressures (>100 kbar = 10 GPa) and temperatures (> 1200°C) present during hypervelocity meteorite impact into quartz-bearing rock. Stishovite may also be synthesized by duplicating these conditions in the laboratory, either isostatically or through shock (see shocked quartz).
owl:sameAs: dbr:Stishovite
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n8:wikiPageUsesTemplate: n9: n20: n21:
n25:: Mineral
n24:: 94
n17:: 110
n14:: 428
n15:: Stishovite
n22:: n23:
n12:: 1650.0
n11:: Clear ; also see Varieties
n16:: Transparent to translucent
n26:: nω = 1.81
n18:abstract: The only known occurrences of stishovite in nature formed at the very high shock pressures (>100 kbar = 10 GPa) and temperatures (> 1200°C) present during hypervelocity meteorite impact into quartz-bearing rock. Stishovite may also be synthesized by duplicating these conditions in the laboratory, either isostatically or through shock (see shocked quartz).