High-pressure polymetamorphic garnet growth in eclogites from the Mariánske Lázně Complex (Bohemian Massif)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F12%3A10126229" target="_blank" >RIV/00216208:11310/12:10126229 - isvavai.cz</a>
Result on the web
<a href="http://eurjmin.geoscienceworld.org/content/24/3/483.full" target="_blank" >http://eurjmin.geoscienceworld.org/content/24/3/483.full</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1127/0935-1221/2012/0024-2184" target="_blank" >10.1127/0935-1221/2012/0024-2184</a>
Alternative languages
Result language
angličtina
Original language name
High-pressure polymetamorphic garnet growth in eclogites from the Mariánske Lázně Complex (Bohemian Massif)
Original language description
The Mariánské-Lázně Complex is a Cambro-Ordovician terrane with metabasites of oceanic-crust affinity and tectonically emplaced between the Saxothuringian Zone and the Teplá-Barrandian Unit (western part of the Bohemian Massif). It is formed by amphibolite (retrogressed after eclogite), serpentinized peridotite, coronitic metagabbro with paragneiss, and felsic orthogneiss. Available geochronological data support Variscan ages for the eclogite-facies metamorphism and subsequent amphibolite-facies reequilibration. Garnet crystals with multi-stage growth features in eclogite were studied to analyse the relation of their chemical zoning with pressure-temperature (P-T) changes and/or reactions among coexisting phases during metamorphism. The core garnet hashighly contrasted compositions with high Mg and low Ca compared to the surrounding host-garnet crystal. Compositional zoning and crystallographic orientation of the garnet showed that the cores and rims were formed during two different m
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
<a href="/en/project/GAP210%2F10%2F0249" target="_blank" >GAP210/10/0249: Early convergence and exhumation history of ultrahigh-pressure lithologies in the Variscan orogen</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2012
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
European Journal of Mineralogy
ISSN
0935-1221
e-ISSN
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Volume of the periodical
24
Issue of the periodical within the volume
3
Country of publishing house
DE - GERMANY
Number of pages
15
Pages from-to
483-497
UT code for WoS article
000304726100008
EID of the result in the Scopus database
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