2008
Sedimentological and palaeocological records of the evolution of the south-western part of the Carpathian Foredeep (Czech Republic) during the Early Badenian
NEHYBA, Slavomír, Pavla PETROVÁ-TOMANOVÁ a Kamil ZAGORŠEKZákladní údaje
Originální název
Sedimentological and palaeocological records of the evolution of the south-western part of the Carpathian Foredeep (Czech Republic) during the Early Badenian
Název česky
Sedimentologický a palaeocologický záznam vývoje jihozápadní části karpatské předhlubně (Česká republika) během spodního badenu
Autoři
NEHYBA, Slavomír (203 Česká republika, garant), Pavla PETROVÁ-TOMANOVÁ (203 Česká republika) a Kamil ZAGORŠEK (203 Česká republika)
Vydání
Geological Quarterly, Warszawa, 2008, 1641-7291
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Polsko
Utajení
není předmětem státního či obchodního tajemství
Impakt faktor
Impact factor: 0.892
Kód RIV
RIV/00216224:14310/08:00025887
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000254925500004
Klíčová slova anglicky
Carpathian Foredeep- Early Badenian- sedimentology- palaeoecology- depositional environment- foraminifers- bryozoans
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 2. 7. 2009 08:24, prof. RNDr. Slavomír Nehyba, Dr.
V originále
The depositional environment of southern part of the Carpathian Foredeep in the Czech Republic was studied in two boreholes using sedimentological and palaeontological methods. Eight lithofacies were recognised within the studied cores of Early Badenian deposits forming two facies associations i.e. deposits of coarse grained Gilbert delta and offshore deposits. Assemblages of foraminifers document age of the Early Badenian (Middle Miocene). Two types of assemblages were recognised: 1. primary taphocoenoses showing original environment of sedimentation, i. e. environment of deeper sublittoral (circalittoral) with low to normal oxygen bottom conditions taking in deep water euryoxibiont foraminifers, numerous planktonic foraminifers, agglutinated ones and mixed assemblages of deep and shallow water foraminifers, 2. secondary taphocoenoses of shallower sublittoral (infralittoral) redeposited into the basin by gravity currents. These assemblages contain shallow water foraminifers coupled with numerous highly diversified bryozoans.
Česky
The depositional environment of southern part of the Carpathian Foredeep in the Czech Republic was studied in two boreholes using sedimentological and palaeontological methods. Eight lithofacies were recognised within the studied cores of Early Badenian deposits forming two facies associations i.e. deposits of coarse grained Gilbert delta and offshore deposits. Assemblages of foraminifers document age of the Early Badenian (Middle Miocene). Two types of assemblages were recognised: 1. primary taphocoenoses showing original environment of sedimentation, i. e. environment of deeper sublittoral (circalittoral) with low to normal oxygen bottom conditions taking in deep water euryoxibiont foraminifers, numerous planktonic foraminifers, agglutinated ones and mixed assemblages of deep and shallow water foraminifers, 2. secondary taphocoenoses of shallower sublittoral (infralittoral) redeposited into the basin by gravity currents. These assemblages contain shallow water foraminifers coupled with numerous highly diversified bryozoans.
Návaznosti
| MSM0021622412, záměr |
|