Kumdykolite, kokchetavite, and cristobalite crystallized in nanogranites from 
felsic granulites, Orlica-Snieznik Dome (Bohemian Massif): not an evidence for 
ultrahigh-pressure conditions

Ferrero, Silvio; Ziemann, Martin A.; Angel, Ross J.; O’Brien, Patrick J.; Wunder, B.

doi:10.1007/s00410-015-1220-x

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Kumdykolite, kokchetavite, and cristobalite crystallized in nanogranites from felsic granulites, Orlica-Snieznik Dome (Bohemian Massif): not an evidence for ultrahigh-pressure conditions

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Ferrero, Silvio
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Ziemann, Martin A.
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Angel, Ross J.
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O’Brien, Patrick J.
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Wunder, B.
3.3 Chemistry and Physics of Earth Materials, 3.0 Geodynamics and Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Ferrero, S., Ziemann, M. A., Angel, R. J., O’Brien, P. J., Wunder, B. (2016): Kumdykolite, kokchetavite, and cristobalite crystallized in nanogranites from felsic granulites, Orlica-Snieznik Dome (Bohemian Massif): not an evidence for ultrahigh-pressure conditions. - Contributions to Mineralogy and Petrology, 171, 3.
https://doi.org/10.1007/s00410-015-1220-x

Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_1397941

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