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Detail publikace
KRMÍČEK, L., CEMPÍREK, J., HAVLÍN, A., PŘICHYSTAL, A., HOUZAR, S., KRMÍČKOVÁ, M., GADAS, P.
Originální název
Mineralogy and petrogenesis of a Ba-Ti-Zr-rich peralkaline dyke from Šebkovice (Czech Republic): Recognition of the most lamproitic Variscan intrusion
Typ
článek v časopise - ostatní, Jost
Jazyk
angličtina
Originální abstrakt
A peralkaline, ultrapotassic dyke found at Šebkovice is a mineralogically extreme member of a dyke swarm occurring along the SE border of the Moldanubian Region of the Bohemian Massif. The dyke shows a simple zoning with a very fine-grained marginal zone grading into a medium-grained central zone. It has a primary mineral assemblage of microcline and potassic amphiboles with accessory apatite and altered phlogopite. The core of the dyke and late veinlets contain unique late- to post-magmatic Ba-Ti-Zr-bearing mineral assemblages of baotite, henrymeyerite, titanite, rutile, benitoite and bazirite. In terms of a mineralogical-genetic classification, the Šebkovice dyke can be considered as a new high-silica variety of lamproite and represents a unique expression of post-collisional potassic magmatism on the south-eastern border of the Bohemian Massif. In terms of the modern classification of lamproites, the Šebkovice dyke is the first lamproite recognised in the Variscan orogenic belt.
Klíčová slova
Lamproite; Potassic amphibole; Baotite; Henrymeyerite; Benitoite; Bazirite
Autoři
Rok RIV
2011
Vydáno
31. 1. 2011
Nakladatel
Elsevier
Místo
Amsterdam
ISSN
0024-4937
Periodikum
LITHOS
Ročník
121
Číslo
1
Stát
Norské království
Strany od
74
Strany do
86
Strany počet
13
BibTex
@article{BUT50735, author="Michaela {Sluková}", title="Mineralogy and petrogenesis of a Ba-Ti-Zr-rich peralkaline dyke from Šebkovice (Czech Republic): Recognition of the most lamproitic Variscan intrusion", journal="LITHOS", year="2011", volume="121", number="1", pages="74--86", issn="0024-4937" }