Brunovistulian Terrane (Central Europe) and Istanbul Zone (NW
Turkey): Late Proterozoic and Paleozoic tectonostratigraphic
development and paleogeography

J 2003

Brunovistulian Terrane (Central Europe) and Istanbul Zone (NW Turkey): Late Proterozoic and Paleozoic tectonostratigraphic development and paleogeography

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

Základní údaje

Originální název

Brunovistulian Terrane (Central Europe) and Istanbul Zone (NW Turkey): Late Proterozoic and Paleozoic tectonostratigraphic development and paleogeography

Autoři

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

Vydání

Geologica Carpathica, 2003, 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: 0.397

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/03:00008820

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

: Brunovistulicum; Istanbul Zone; terranes; paleogeography; late Proterozoic; Paleozoic.

Štítky

: Brunovistulicum, Istanbul Zone, late Proterozoic, Paleogeography, Paleozoic., terranes

Změněno: 21. 7. 2003 09:09, 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 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 central Malopolska, Brunovistulian and Moesian terranes correlate well with the Scythian Platform. In the Istanbul Zone the presence of the pre-Ordovician sedimentary sequences has not been confirmed and may be only anticipated. In Paleozoic the best fit was attained in the Devonian-Carboniferous interval.The sedimentary record in the Zonguldak and Istanbul terranes closely compares to the Moravian Karst and Ludmirov facies developments of the Brunovistulian Terrane. The correlation is reinforced by a good fit of main Variscan deformation phases attributed both in the Brunovistulian Terrane and the Istanbul Zone to the late Visean-early Namurian and Westphalian-Stephanian intervals. This supports, together with the paleobiogeographic data, the interpretation that the Istanbul and Zonguldak terranes can be regarded as counterparts of the Rhenohercynian and Subvariscan Zone in Central Europe. The Istanbul Zone is 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; Jaromír LEICHMANN; Ondřej BÁBEK a Rostislav MELICHAR. Brunovistulian Terrane (Central Europe) and Istanbul Zone (NW Turkey): Late Proterozoic and Paleozoic tectonostratigraphic development and paleogeography. Geologica Carpathica. 2003, roč. 54, č. 3, s. 139-152, 13 s. ISSN 1335-0552.

@article{487962,
   author = {Kalvoda, Jiří and Leichmann, Jaromír and Bábek, Ondřej and Melichar, Rostislav},
   article_number = {3},
   keywords = {: Brunovistulicum; Istanbul Zone; terranes; paleogeography; late Proterozoic; Paleozoic.},
   language = {eng},
   issn = {1335-0552},
   journal = {Geologica Carpathica},
   title = {Brunovistulian Terrane (Central Europe) and Istanbul Zone (NW Turkey): Late Proterozoic and Paleozoic tectonostratigraphic development and paleogeography},
   volume = {54},
   year = {2003}
}

TY  - JOUR
ID  - 487962
AU  - Kalvoda, Jiří - Leichmann, Jaromír - Bábek, Ondřej - Melichar, Rostislav
PY  - 2003
TI  - Brunovistulian Terrane (Central Europe) and Istanbul Zone (NW Turkey): Late Proterozoic and Paleozoic tectonostratigraphic development and paleogeography
JF  - Geologica Carpathica
VL  - 54
IS  - 3
SP  - 139-152
EP  - 139-152
SN  - 13350552
KW  - : Brunovistulicum
KW  - Istanbul Zone
KW  - terranes
KW  - paleogeography
KW  - late Proterozoic
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 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 central Malopolska, Brunovistulian and Moesian terranes correlate well with the Scythian Platform. In the Istanbul Zone the presence of the pre-Ordovician sedimentary sequences has not been confirmed and may be only anticipated. In Paleozoic the best fit was attained in the Devonian-Carboniferous interval.The sedimentary record in the Zonguldak and Istanbul terranes closely compares to the Moravian Karst and Ludmirov facies developments of the Brunovistulian Terrane. The correlation is reinforced by a good fit of main Variscan deformation phases attributed both in the Brunovistulian Terrane and the Istanbul Zone to the late Visean-early Namurian and Westphalian-Stephanian intervals. This supports, together with the paleobiogeographic data, the interpretation that the Istanbul and Zonguldak terranes can be regarded as counterparts of the Rhenohercynian and Subvariscan Zone in Central Europe. The Istanbul Zone is juxtaposed against the Sakarya Zone viewed as a part of the Armorican Terrane Assemblage.
ER  -

KALVODA, Jiří; Jaromír LEICHMANN; Ondřej BÁBEK a Rostislav MELICHAR. Brunovistulian Terrane (Central Europe) and Istanbul Zone (NW Turkey): Late Proterozoic and Paleozoic tectonostratigraphic development and paleogeography. \textit{Geologica Carpathica}. 2003, roč.~54, č.~3, s.~139-152, 13 s. ISSN~1335-0552.

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