The Pressure?Temperature Path and the Origin of Phlogopite in Spinel?Garnet Peridotites from the Blanský les Massif of the Moldanubian Zone, Czech Republic
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F09%3A00335101" target="_blank" >RIV/67985831:_____/09:00335101 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
The Pressure?Temperature Path and the Origin of Phlogopite in Spinel?Garnet Peridotites from the Blanský les Massif of the Moldanubian Zone, Czech Republic
Original language description
A new lithotype of peridotite, phlogopite- and apatite-bearing spinel?garnet peridotite, associated with leucocratic granulite, has been recognized at the Plešovice quarry in the Gföhl Unit within the Moldanubian Zone of the Bohemian Massif, Czech Republic. There are three equilibrium stages in the Pleovice peridotite. The existence of Stage I, the precursor spinel garnet peridotite stage, is supported by the presence of an aluminous (Al2O3 3,0 wt %) orthopyroxene megacryst in the matrix. The minimum temperature of Stage I was estimated to be 1020 15°C.
Czech name
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Czech description
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Classification
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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Result continuities
Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2009
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Petrology
ISSN
0022-3530
e-ISSN
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Volume of the periodical
50
Issue of the periodical within the volume
10
Country of publishing house
GB - UNITED KINGDOM
Number of pages
33
Pages from-to
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UT code for WoS article
000271577800001
EID of the result in the Scopus database
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