Upper Devonian-Lower Carboniferous foraminiferal
paleobiogeography and Perigondwana terranes at the
Baltica-Gondwana interface

J 2001

Upper Devonian-Lower Carboniferous foraminiferal paleobiogeography and Perigondwana terranes at the Baltica-Gondwana interface

KALVODA, Jiří

Základní údaje

Originální název

Upper Devonian-Lower Carboniferous foraminiferal paleobiogeography and Perigondwana terranes at the Baltica-Gondwana interface

Autoři

KALVODA, Jiří

Vydání

Geologica Carpathica, Bratislava, Slovak Akademy of Science, 2001, 1335-0552

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Slovensko

Utajení

není předmětem státního či obchodního tajemství

Impakt faktor

Impact factor: 0.167

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/01:00004672

Organizační jednotka

Přírodovědecká fakulta

UT WoS

000171603200002

Klíčová slova anglicky

Foraminifers; Upper Devonian; Lower Carboniferous; Brunovistulian terrane; Moesian terrane; Zonguldak terrane

Štítky

Brunovistulian terrane, foraminifers, Lower Carboniferous, Moesian terrane, Upper Devonian, Zonguldak terrane

Změněno: 16. 11. 2001 15:12, prof. RNDr. Jiří Kalvoda, CSc.

Anotace

V originále

A new paleobiogeographic subdivision of the Perigondwana terranes is based on the study of Upper Devonian and Lower Carboniferous calcareous foraminifers. The Brunovistulian, Moesian and Zonguldak Terranes in Central and SE Europe and Asia Minor (the Brunovistulian group of terranes) show close paleobiogeographic relationships to the East European foraminiferal association. Consequently, they are regarded as a part of the Fennosarmatian Province which represented a center of the diversification for most groups of Upper Devonian and Lower Carboniferous calcareous foraminifers. A lower degree of similarity with the East European Platform can be distinguished in the East Avalonian foraminiferal fauna while that of the Armorican group of terranes displays distinct differences constituting the separate Armorican Province. The results obtained support the idea that the Brunovistulian group of terranes formed the southern margin of Laurussia which was colliding with the Armorican group of terranes during the Variscan orogeny. In this respect, Brunovistulian group of terranes held a geotectonic position similar to that of East Avalonia even though the accretionary history of the terranes was different.

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. Upper Devonian-Lower Carboniferous foraminiferal paleobiogeography and Perigondwana terranes at the Baltica-Gondwana interface. Geologica Carpathica. Bratislava: Slovak Akademy of Science, 2001, roč. 52, č. 4, s. 205-419. ISSN 1335-0552.

@article{376491,
   author = {Kalvoda, Jiří},
   article_location = {Bratislava},
   article_number = {4},
   keywords = {Foraminifers; Upper Devonian; Lower Carboniferous; Brunovistulian terrane; Moesian terrane; Zonguldak terrane},
   language = {eng},
   issn = {1335-0552},
   journal = {Geologica Carpathica},
   title = {Upper Devonian-Lower Carboniferous foraminiferal paleobiogeography and Perigondwana terranes at the Baltica-Gondwana interface},
   volume = {52},
   year = {2001}
}

TY  - JOUR
ID  - 376491
AU  - Kalvoda, Jiří
PY  - 2001
TI  - Upper Devonian-Lower Carboniferous foraminiferal paleobiogeography and Perigondwana terranes at the Baltica-Gondwana interface
JF  - Geologica Carpathica
VL  - 52
IS  - 4
SP  - 205
EP  - 205
PB  - Slovak Akademy of Science
SN  - 13350552
KW  - Foraminifers
KW  - Upper Devonian
KW  - Lower Carboniferous
KW  - Brunovistulian terrane
KW  - Moesian terrane
KW  - Zonguldak terrane
N2  - A new paleobiogeographic subdivision of the Perigondwana terranes is based on the study of Upper Devonian and Lower Carboniferous calcareous foraminifers. The Brunovistulian, Moesian and Zonguldak Terranes in Central and SE Europe and Asia Minor (the Brunovistulian group of terranes) show close paleobiogeographic relationships to the East European foraminiferal association. Consequently, they are regarded as a part of the Fennosarmatian Province which represented a center of the diversification for most groups of Upper Devonian and Lower Carboniferous calcareous foraminifers. A lower degree of similarity with the East European Platform can be distinguished in the East Avalonian foraminiferal fauna while that of the Armorican group of terranes displays distinct differences constituting the separate Armorican Province. The results obtained support the idea that the Brunovistulian group of terranes formed the southern margin of Laurussia which was colliding with the Armorican group of terranes during the Variscan orogeny. In this respect, Brunovistulian group of terranes held a geotectonic position similar to that of East Avalonia even though the accretionary history of the terranes was different.
ER  -

KALVODA, Jiří. Upper Devonian-Lower Carboniferous foraminiferal paleobiogeography and Perigondwana terranes at the Baltica-Gondwana interface. \textit{Geologica Carpathica}. Bratislava: Slovak Akademy of Science, 2001, roč.~52, č.~4, s.~205-419. ISSN~1335-0552.

Přehled o publikaci