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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F08%3A00028036%21RIV10-MSM-14310___
rdf:type
n15:Vysledek skos:Concept
dcterms:description
The Brno Batholith, a part of the larger Brunovistulian Unit, consists of three genetically independent complexes, Western Granitoid Complex (part of the Thaya Terrane), Ophiolite Belt (formerly Metabasite Zone or Central Basic Belt), and Eastern Granitoid Complex (part of the Slavkov Terrane). The field with geochronological evidence indicate younger age of both granitoid complexes compared with the ophiolite. The composition of the Eastern Granitoid Complex (not newly studied in this paper) points to a relatively primitive Cadomian volcanic-arc environment. The Ophiolite Belt comprises a tilted segment of an almost complete metamorphosed ophiolite sequence with lithologically and geochemically obvious suprasubduction signature. Three main granite suites, with distinct S, I, and A type affinities, are exposed in the Western Granitoid Complex. The Brno Batholith, a part of the larger Brunovistulian Unit, consists of three genetically independent complexes, Western Granitoid Complex (part of the Thaya Terrane), Ophiolite Belt (formerly Metabasite Zone or Central Basic Belt), and Eastern Granitoid Complex (part of the Slavkov Terrane). The field with geochronological evidence indicate younger age of both granitoid complexes compared with the ophiolite. The composition of the Eastern Granitoid Complex (not newly studied in this paper) points to a relatively primitive Cadomian volcanic-arc environment. The Ophiolite Belt comprises a tilted segment of an almost complete metamorphosed ophiolite sequence with lithologically and geochemically obvious suprasubduction signature. Three main granite suites, with distinct S, I, and A type affinities, are exposed in the Western Granitoid Complex.
dcterms:title
The Brno Batholith: an insight into the magmatic and metamorphic evolution of the Cadomian Brunovistulian Unit,eastern margin of the Bohemian Massif The Brno Batholith: an insight into the magmatic and metamorphic evolution of the Cadomian Brunovistulian Unit,eastern margin of the Bohemian Massif
skos:prefLabel
The Brno Batholith: an insight into the magmatic and metamorphic evolution of the Cadomian Brunovistulian Unit,eastern margin of the Bohemian Massif The Brno Batholith: an insight into the magmatic and metamorphic evolution of the Cadomian Brunovistulian Unit,eastern margin of the Bohemian Massif
skos:notation
RIV/00216224:14310/08:00028036!RIV10-MSM-14310___
n3:aktivita
n16:Z
n3:aktivity
Z(MSM0021622412)
n3:cisloPeriodika
1
n3:dodaniDat
n4:2010
n3:domaciTvurceVysledku
n8:6504507
n3:druhVysledku
n13:J
n3:duvernostUdaju
n18:S
n3:entitaPredkladatele
n17:predkladatel
n3:idSjednocenehoVysledku
358508
n3:idVysledku
RIV/00216224:14310/08:00028036
n3:jazykVysledku
n14:eng
n3:klicovaSlova
Brno Batholith; Brunovistulicum; granites; ophiolites; Gondwana; petrology
n3:klicoveSlovo
n7:granites n7:ophiolites n7:petrology n7:Brno%20Batholith n7:Brunovistulicum n7:Gondwana
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[672EACD88520]
n3:nazevZdroje
Journal of Geosciences
n3:obor
n10:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
2
n3:rokUplatneniVysledku
n4:2008
n3:svazekPeriodika
53
n3:tvurceVysledku
Leichmann, Jaromír Hoeck, Volker
n3:zamer
n12:MSM0021622412
s:issn
1802-6222
s:numberOfPages
24
n6:organizacniJednotka
14310