Geochemistry of subsurface Precambrian plutonic rocks from the Brunovistulian complex in the Bohemian massif, Czechoslovakia

1993 ◽  
Vol 62 (1-2) ◽  
pp. 103-125 ◽  
Author(s):  
E. Jelínek ◽  
A. Dudek
Lithos ◽  
2010 ◽  
Vol 115 (1-4) ◽  
pp. 163-176 ◽  
Author(s):  
Jana Kotková ◽  
Urs Schaltegger ◽  
Jaromír Leichmann

1995 ◽  
Vol 90 (9) ◽  
pp. 297-309 ◽  
Author(s):  
Keisuke SAHEKI ◽  
Masatoshi SHIBA ◽  
Tetsumaru ITAYA ◽  
Hitoshi ONUKI
Keyword(s):  

2014 ◽  
Vol 64 (4) ◽  
pp. 367-392 ◽  
Author(s):  
Karolína Lajblová ◽  
Petr Kraft

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.


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