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Received: 13 March, 2016
Accepted: 7 March, 2017
Online: 25 March 2017
H. Editor: V. Kachlík
Responsible Editorial Board
 
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Keywords:
Bohemian Massif
Moldanubian Zone
geochemistry
skarn
mineralogy
diorite pegmatite
 
More articles on Evolved felsic igneous systems and granitic pegmatites
 

Original paper

David Buriánek, Stanislav Houzar, Lukáš Krmíček, Jaroslav Šmerda

Origin of the pegmatite veins within the skarn body at Vevčice near Znojmo (Gföhl Unit, Moldanubian Zone)

Journal of Geosciences, volume 62 (2017), issue 1, 1 - 23

DOI: http://doi.org/10.3190/jgeosci.234


  Abstract References Map Affiliations

David Buriánek

Czech Geological Survey, Leitnerova 22, 658 59 Brno, Czech Republic

Stanislav Houzar

Department of Mineralogy and Petrography, Moravian Museum, Zelný trh 6, 674 01 Brno, Czech Republic

Lukáš Krmíček

Faculty of Civil Engineering, AdMaS Centre, Brno University of Technology, Veveří 95, 602 00 Brno, Czech Republic

Institute of Geology of the Czech Academy of Sciences, v. v .i., Rozvojová 269, 165 02 Prague 6, Czech Republic

Jaroslav Šmerda

South Moravian Museum in Znojmo, Přemyslovců 8/129, 669 45 Znojmo, Czech Republic

Journal of Geosciences, Published by © Czech Geological Society, with support from the Czech Geological Survey.
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