Brunovistulian terrane (Czech Republic, Middle European
Variscides) and Lower Carboniferous Paleobiogeography

D 2000

Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography

KALVODA, Jiří

Základní údaje

Originální název

Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography

Autoři

KALVODA, Jiří

Vydání

Evora, I COngresso Ibérico de Paléontología, XVI Jornadas de la Sociedad Espanola de Paleontologia, Livro de Resumos, s. 239-239, 2000

Nakladatel

Universidade de Evora

Další údaje

Jazyk

angličtina

Typ výsledku

Stať ve sborníku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Portugalsko

Utajení

není předmětem státního či obchodního tajemství

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/00:00002600

Organizační jednotka

Přírodovědecká fakulta

ISBN

972-778-026-1

Klíčová slova anglicky

Brunovistulian terrane; paleobiogeography; Lower Carboniferous

Štítky

Brunovistulian terrane, Lower Carboniferous, paleobiogeography

Změněno: 20. 12. 2000 12:30, prof. RNDr. Jiří Kalvoda, CSc.

Anotace

V originále

The Brunovistulian Terrane was similarly as the Eastern Avalonia Terrane a part of the Panafrican (Cadomian) Gondwana margin. The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentation of Gondwana while the faunistic record of Cambrian fauna shows close relation to Baltica (Belka et al. 1999). It is assumed that the Brunovistulian Terrane was amalgamated to the southeastern margin of Baltica and dextral translation is characteristic for its contact with northern Malopolska Terrane along the Krakow-Lubliniec Zone (Grygar, Vavro 1995). Thus the Brunovistulian Terrane was amalgamated to Baltica similarly as the Eastern Avalonia Terrane in the Lower Paleozoic, however, the Eastern Avalonian Terrane shows, contrary to the Brunovistulian Terrane, predominant sinistral translation. This differencies between the eastern and western part of the Middle European Variscides may have continued in the Upper Paleozoic. While the collision of the Armorican Terrane with Eastern Avalonian margin of Laurussia took place in the west, the complicated interaction of the Brunovistulian margin of Laurussia with both Armorican and Moldanubian terranes took place in the east. Summarizing we assume more important role of terranes in the structure of the Middle European Variscides analogous to the evolution of Appalachians.

Návaznosti

GA205/99/1640, projekt VaV

Název: Paleobiogeografická evoluce foraminiferové fauny na kontaktu Gondwany a Baltiky v nejvyšším devonu a spodním karbonu

Investor: Grantová agentura ČR, Paleobiogeografická evoluce foraminiferové fauny na kontaktu Gondwany a Baltiky v nejvyšším devonu a spodním karbonu

MSM 143100004, záměr

Název: Geologické procesy a jejich environmentální vyústění - styk variscid a alpid

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Geologické procesy a jejich environmentální vyústění - styk variscid a alpid

Citovat

KALVODA, Jiří. Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography. In I COngresso Ibérico de Paléontología, XVI Jornadas de la Sociedad Espanola de Paleontologia, Livro de Resumos. Evora: Universidade de Evora, 2000, s. 239. ISBN 972-778-026-1.

@inproceedings{344859,
   author = {Kalvoda, Jiří},
   address = {Evora},
   booktitle = {I COngresso Ibérico de Paléontología, XVI Jornadas de la Sociedad Espanola de Paleontologia, Livro de Resumos},
   keywords = {Brunovistulian terrane; paleobiogeography; Lower Carboniferous},
   language = {eng},
   location = {Evora},
   isbn = {972-778-026-1},
   pages = {239-239},
   publisher = {Universidade de Evora},
   title = {Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography},
   year = {2000}
}

TY  - CONF
ID  - 344859
AU  - Kalvoda, Jiří
PY  - 2000
TI  - Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography
PB  - Universidade de Evora
CY  - Evora
SN  - 9727780261
KW  - Brunovistulian terrane
KW  - paleobiogeography
KW  - Lower Carboniferous
N2  - The Brunovistulian Terrane was similarly as the Eastern Avalonia Terrane a part of the Panafrican (Cadomian) Gondwana margin. The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentation of Gondwana while the faunistic record of Cambrian fauna shows close relation to Baltica (Belka et al. 1999). It is assumed that the Brunovistulian Terrane was amalgamated to the southeastern margin of Baltica and dextral translation is characteristic for its contact with northern Malopolska Terrane along the Krakow-Lubliniec Zone (Grygar, Vavro 1995). Thus the Brunovistulian Terrane was amalgamated to Baltica similarly as the Eastern Avalonia Terrane in the Lower Paleozoic, however, the Eastern Avalonian Terrane shows, contrary to the Brunovistulian Terrane, predominant sinistral translation. This differencies between the eastern and western part of the Middle European Variscides may have continued in the Upper Paleozoic. While the collision of the Armorican Terrane with Eastern Avalonian margin of Laurussia took place in the west, the complicated interaction of the Brunovistulian margin of Laurussia with both Armorican and Moldanubian terranes took place in the east. Summarizing we assume more important role of terranes in the structure of the Middle European Variscides analogous to the evolution of Appalachians.
ER  -

KALVODA, Jiří. Brunovistulian terrane (Czech Republic, Middle European Variscides) and Lower Carboniferous Paleobiogeography. In \textit{I COngresso Ibérico de Paléontología, XVI Jornadas de la Sociedad Espanola de Paleontologia, Livro de Resumos}. Evora: Universidade de Evora, 2000, s.~239. ISBN~972-778-026-1.

Přehled o publikaci