Intermediate granulite produced by transformation of eclogite at a felsic granulite contact, in Blanský les, Bohemian Massif

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000156" target="_blank" >RIV/00025798:_____/14:00000156 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11310/14:10218415

Výsledek na webu

<a href="http://onlinelibrary.wiley.com/doi/10.1111/jmg.12079/abstract" target="_blank" >http://onlinelibrary.wiley.com/doi/10.1111/jmg.12079/abstract</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1111/jmg.12079" target="_blank" >10.1111/jmg.12079</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Intermediate granulite produced by transformation of eclogite at a felsic granulite contact, in Blanský les, Bohemian Massif

Popis výsledku v původním jazyce

Layers or bodies of intermediate granulite on scales from a centimetre to a hundred metres occur commonly within the felsic granulite massifs of the Bohemian Massif. Their origin is enigmatic in that they commonly have complex microstructures that are difficult to interpret, and therefore even the sequence of crystallization of minerals is uncertain. At Kleť, in the Blanský les massif, there is a revealing outcrop in a low-strain zone in which it is clear that intermediate granulite can form by the interaction of felsic granulite with eclogite. The eclogite, retains garnet from its eclogite heritage, the grains at least partially isolated from the matrix by a plagioclase corona. The original omphacite-dominated matrix of the eclogite now consists of recrystallized diopsidic clinopyroxene, orthopyroxene and plagioclase, with minor brown amphibole and quartz. The modification of the eclogite is dominated by the addition of just K2O and H2O, rather than all the elements that would be invo

Název v anglickém jazyce

Intermediate granulite produced by transformation of eclogite at a felsic granulite contact, in Blanský les, Bohemian Massif

Popis výsledku anglicky

Layers or bodies of intermediate granulite on scales from a centimetre to a hundred metres occur commonly within the felsic granulite massifs of the Bohemian Massif. Their origin is enigmatic in that they commonly have complex microstructures that are difficult to interpret, and therefore even the sequence of crystallization of minerals is uncertain. At Kleť, in the Blanský les massif, there is a revealing outcrop in a low-strain zone in which it is clear that intermediate granulite can form by the interaction of felsic granulite with eclogite. The eclogite, retains garnet from its eclogite heritage, the grains at least partially isolated from the matrix by a plagioclase corona. The original omphacite-dominated matrix of the eclogite now consists of recrystallized diopsidic clinopyroxene, orthopyroxene and plagioclase, with minor brown amphibole and quartz. The modification of the eclogite is dominated by the addition of just K2O and H2O, rather than all the elements that would be invo

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Metamorphic Geology

ISSN

0263-4929

e-ISSN

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Svazek periodika

32

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

23

Strana od-do

347-370

Kód UT WoS článku

000333540600024

EID výsledku v databázi Scopus

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