High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic)

Lithos ◽  
2011 ◽  
Vol 125 (1-2) ◽  
pp. 641-658 ◽  
Author(s):  
Radmila Nahodilová ◽  
Shah Wali Faryad ◽  
David Dolejš ◽  
Peter Tropper ◽  
Jürgen Konzett
Keyword(s):  
High Pressure ◽  
Czech Republic ◽  
Partial Melting ◽  
Bohemian Massif

A vestige of very high-pressure (ca. 28 kbar) metamorphism in the Variscan Bohemian Massif, Czech Republic

1997 ◽  
Vol 9 (5) ◽  
pp. 1017-1034 ◽  
Author(s):  
Jana Kotková ◽  
Simon L. Harley ◽  
Milan Fišera
Keyword(s):  
High Pressure ◽  
Czech Republic ◽  
Bohemian Massif ◽  
Very High

scholarly journals Evidence for partial melting of eclogite from the Moldanubian Zone of the Bohemian Massif, Czech Republic

2016 ◽  
Vol 111 (6) ◽  
pp. 405-419 ◽  
Author(s):  
Takahiro MIYAZAKI ◽  
Daisuke NAKAMURA ◽  
Akihiro TAMURA ◽  
Martin SVOJTKA ◽  
Shoji ARAI ◽  
...  
Keyword(s):  
Czech Republic ◽  
Partial Melting ◽  
Bohemian Massif ◽  
Moldanubian Zone

Sm-Nd and U-Pb dating of high-pressure granulites from the Zlote and Rychleby Mts (Bohemian Massif, Poland and Czech Republic)

2005 ◽  
Vol 23 (3) ◽  
pp. 133-145 ◽  
Author(s):  
U. LANGE ◽  
M. BROCKER ◽  
R. ARMSTRONG ◽  
E. TRAPP ◽  
K. MEZGER
Keyword(s):  
High Pressure ◽  
Czech Republic ◽  
Bohemian Massif

The earliest ostracods from the Ordovician of the Prague Basin, Czech Republic

2014 ◽  
Vol 64 (4) ◽  
pp. 367-392 ◽  
Author(s):  
Karolína Lajblová ◽  
Petr Kraft
Keyword(s):  
Czech Republic ◽  
Bohemian Massif ◽  
Massif Central ◽  
Central European ◽  
Middle Ordovician ◽  
Prague Basin ◽  
Barrandian Area ◽  
Fossil Assemblages ◽  
European Variscides

Abstract The earliest ostracods from the Bohemian Massif (Central European Variscides) have been recorded from the Middle Ordovician of the Prague Basin (Barrandian area), in the upper Klabava Formation, and became an abundant component of fossil assemblages in the overlying Šarka Formation. Both early ostracod associations consist of eight species in total, representing mainly eridostracans, palaeocopids, and binodicopids. The revision, description, or redescription of all species and their distribution in the basin is provided. Their diversification patterns and palaeogeographical relationships to ostracod assemblages from other regions are discussed.

Mollusc successions reveal northward postglacial shifts of Alpine species ranges (Bohemian Massif, Czech Republic)

The Holocene ◽  
2021 ◽  
pp. 095968362110116
Author(s):  
Lucie Juřičková ◽  
Jakub Menšík ◽  
Jitka Horáčková ◽  
Vojen Ložek
Keyword(s):  
Czech Republic ◽  
Bohemian Massif ◽  
Late Glacial ◽  
Glacial Refugia ◽  
Land Snails ◽  
Glacial Refugium ◽  
Local Climate ◽  
The Alps ◽  
Species Groups ◽  
Late Glacial And Holocene

The Alps are an important hotspot of species diversity and endemism, as well as a presumed glacial refugium of several species’ groups including land snails. The recent ranges of Alpine endemics are well known, but their fluctuations during the postglacial period mirroring local climate changes are understudied. By analysing five Late Glacial and Holocene mollusc successions from two areas in the southernmost part of the Bohemian Massif (Czech Republic) situated about 100 km north of the Alps, we reveal details of these fluctuations. The Alpine endemic rocky dweller Chilostoma achates had reached the southern part of the Bohemian Massif already in the Late Glacial and disappeared in the Mid-Holocene canopy forest optimum. On the contrary, the northern boundaries of Alpine canopy forest epigeic snails extended further north than today at the turn of the Middle and Late-Holocene, pointing to a more favourable forest microclimate. The earliest known occurrences of several temperate canopy forest central European species, especially Causa holosericea and Discus perspectivus, imply the role of different areas in the Alps as their glacial refugia.

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