Late Proterozoic - Paleozoic Tectonostratigraphic Development
and Paleogeography of Brunivistulian Terrane and Comparison
with other Terranes at the SE Margin of Baltica-Laurussia

J 2003

Late Proterozoic - Paleozoic Tectonostratigraphic Development and Paleogeography of Brunivistulian Terrane and Comparison with other Terranes at the SE Margin of Baltica-Laurussia

KALVODA, Jiří, Rostislav MELICHAR, Ondřej BÁBEK a Jaromír LEICHMANN

Základní údaje

Originální název

Late Proterozoic - Paleozoic Tectonostratigraphic Development and Paleogeography of Brunivistulian Terrane and Comparison with other Terranes at the SE Margin of Baltica-Laurussia

Autoři

KALVODA, Jiří (203 Česká republika, garant), Rostislav MELICHAR (203 Česká republika), Ondřej BÁBEK (203 Česká republika) a Jaromír LEICHMANN (203 Česká republika)

Vydání

Journal of the Czech Geological Society, Praha, 2003, 1210-8197

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10500 1.5. Earth and related environmental sciences

Stát vydavatele

Česká republika

Utajení

není předmětem státního či obchodního tajemství

Kód RIV

RIV/00216224:14310/03:00008843

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

Brunovistulicum; Istanbul Zone; terranes; paleogeography; late Neoproterozoic; Paleozoic.

Štítky

Brunovistulicum, Istanbul Zone, late Neoproterozoic, Paleogeography, Paleozoic., terranes

Změněno: 26. 8. 2003 11:15, prof. RNDr. Jiří Kalvoda, CSc.

Anotace

V originále

There are close similarities between the Brunovistulian Terrane and the Istanbul Zone both in the Neoproterozoic and Paleozoic. The geological structure, lithology and geochronology of the Cadomian Brunovistulicum show a broad fit with the crystalline basement of the Istanbul Zone. Their Gondwana or Baltica affinity is still poorly constrained and remains a matter of discussion. The Vendian and Cambrian sequences recognized in the central Malopolska, Brunovistulian and Moesian terranes correlate well with the Scythian Platform. In the Istanbul Zone the presence of pre-Ordovician sedimentary sequences has not been confirmed and may only be anticipated. In Paleozoic the best fit was attained in the Devonian-Carboniferous. The sedimentary record in the Zonguldak and Istanbul terranes correlates closely to the Moravian Karst and Ludmírov facies developments of the Brunovistulian Terrane. This correlation is reinforced by the good fit of the main Variscan deformation phases attributed in both the Brunovistulian Terrane and the Istanbul Zone to the late Visean-early Namurian and Westphalian-Stephanian intervals. This supports, together with the paleobiogeographical data, the interpretation that the Istanbul and Zonguldak terranes can be regarded as counterparts to the Rhenohercynian and Subvariscan Zone in Central Europe. The Istanbul Zone was juxtaposed against the Sakarya Zone viewed as a part of the Armorican Terrane Assemblage.

Návaznosti

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, Rostislav MELICHAR, Ondřej BÁBEK a Jaromír LEICHMANN. Late Proterozoic - Paleozoic Tectonostratigraphic Development and Paleogeography of Brunivistulian Terrane and Comparison with other Terranes at the SE Margin of Baltica-Laurussia. Journal of the Czech Geological Society. Praha, 2003, roč. 47, č. 3, s. 81-102, 21 s. ISSN 1210-8197.

@article{488155,
   author = {Kalvoda, Jiří and Melichar, Rostislav and Bábek, Ondřej and Leichmann, Jaromír and Melichar, Rostislav and Bábek, Ondřej and Leichmann, Jaromír},
   article_location = {Praha},
   article_number = {3},
   keywords = {Brunovistulicum; Istanbul Zone; terranes; paleogeography; late Neoproterozoic; Paleozoic.},
   language = {eng},
   issn = {1210-8197},
   journal = {Journal of the Czech Geological Society},
   note = {Brunovistulicum, Istanbul Zone, terranes, paleogeography, late Neoproterozoic, Paleozoic.},
   title = {Late Proterozoic - Paleozoic Tectonostratigraphic Development and Paleogeography of Brunivistulian Terrane and Comparison with other Terranes at the SE Margin of Baltica-Laurussia},
   volume = {47},
   year = {2003}
}

TY  - JOUR
ID  - 488155
AU  - Kalvoda, Jiří - Melichar, Rostislav - Bábek, Ondřej - Leichmann, Jaromír - Melichar, Rostislav - Bábek, Ondřej - Leichmann, Jaromír
PY  - 2003
TI  - Late Proterozoic - Paleozoic Tectonostratigraphic Development and Paleogeography of Brunivistulian Terrane and Comparison with other Terranes at the SE Margin of Baltica-Laurussia
JF  - Journal of the Czech Geological Society
VL  - 47
IS  - 3
SP  - 81-102
EP  - 81-102
SN  - 12108197
N1  - Brunovistulicum, Istanbul Zone, terranes, paleogeography, late Neoproterozoic, Paleozoic.
KW  - Brunovistulicum
KW  - Istanbul Zone
KW  - terranes
KW  - paleogeography
KW  - late Neoproterozoic
KW  - Paleozoic.
N2  - There are close similarities between the Brunovistulian Terrane and the Istanbul Zone both in the Neoproterozoic and Paleozoic. The geological structure, lithology and geochronology of the Cadomian Brunovistulicum show a broad fit with the crystalline basement of the Istanbul Zone. Their Gondwana or Baltica affinity is still poorly constrained and remains a matter of discussion. The Vendian and Cambrian sequences recognized in the central Malopolska, Brunovistulian and Moesian terranes correlate well with the Scythian Platform. In the Istanbul Zone the presence of pre-Ordovician sedimentary sequences has not been confirmed and may only be anticipated. In Paleozoic the best fit was attained in the Devonian-Carboniferous. The sedimentary record in the Zonguldak and Istanbul terranes correlates closely to the Moravian Karst and Ludmírov facies developments of the Brunovistulian Terrane. This correlation is reinforced by the good fit of the main Variscan deformation phases attributed in both the Brunovistulian Terrane and the Istanbul Zone to the late Visean-early Namurian and Westphalian-Stephanian intervals. This supports, together with the paleobiogeographical data, the interpretation that the Istanbul and Zonguldak terranes can be regarded as counterparts to the Rhenohercynian and Subvariscan Zone in Central Europe. The Istanbul Zone was juxtaposed against the Sakarya Zone viewed as a part of the Armorican Terrane Assemblage.
ER  -

KALVODA, Jiří, Rostislav MELICHAR, Ondřej BÁBEK a Jaromír LEICHMANN. Late Proterozoic - Paleozoic Tectonostratigraphic Development and Paleogeography of Brunivistulian Terrane and Comparison with other Terranes at the SE Margin of Baltica-Laurussia. \textit{Journal of the Czech Geological Society}. Praha, 2003, roč.~47, č.~3, s.~81-102, 21 s. ISSN~1210-8197.

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