Growth of plagioclase rims around metastable kyanite during decompression of high-pressure felsic granulites (Bohemian Massif)

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F11%3A00000451" target="_blank" >RIV/00025798:_____/11:00000451 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1111/j.1525-1314.2011.00953.x" target="_blank" >http://dx.doi.org/10.1111/j.1525-1314.2011.00953.x</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1111/j.1525-1314.2011.00953.x" target="_blank" >10.1111/j.1525-1314.2011.00953.x</a>

Result language
angličtina
Original language name
Growth of plagioclase rims around metastable kyanite during decompression of high-pressure felsic granulites (Bohemian Massif)
Original language description
Samples of high-pressure felsic granulites from the Bohemian Massif (Variscan belt of Central Europe) characterized by a peak metamorphic (high-pressure) mineral assemblage of garnet?kyanite?plagioclase?K-feldspar?quartz ? biotite show well-developed plagioclase reaction rims around kyanite grains in two microstructural settings. In one setting, kyanite is randomly distributed in the polyphase matrix, whereas in the other setting, it is enclosed within large perthitic K-feldspar. Kyanite is regarded asa relict of the high-pressure metamorphic assemblage that became metastable during transition to a low-pressure overprint.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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