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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F03%3A00008139%21RIV08-MSM-14310___
rdf:type
skos:Concept n12:Vysledek
dcterms:description
Four foraminiferal paleobiogeographic realms are distinguished in the Carboniferous - North Paleotethyan, Perigondwanian, Siberian and North American. The Carboniferous foraminiferal faunas of both the Istanbul and Anatolide-Tauride zones distinctly differ from both Cimmerian terranes (Central Afghanistan, Qiangtang) and Libya and Egypt of the Perigondwana Realm and show close relation to the North Paleotethyan Realm, especially to the Fennosarmatian Province of southeastern Laurussia (Moesian and Scythian platforms) or to the Central Asiatic Province. A model that best fits with available evidence is that the Anatolide-Tauride Zone was either a part or located close to Laurasia in Carboniferous. The Istanbul Zone represents an equivalent of the Rhehohercynian Zone of the Central Europe and can not be compared with Intra-Alpine or south Variscan terranes which may be correlated with the Anatolide-Tauride Zone. Later, in the Permian, the Anatolide -Tauride Zone may has been separated from the Eurasian Four foraminiferal paleobiogeographic realms are distinguished in the Carboniferous - North Paleotethyan, Perigondwanian, Siberian and North American. The Carboniferous foraminiferal faunas of both the Istanbul and Anatolide-Tauride zones distinctly differ from both Cimmerian terranes (Central Afghanistan, Qiangtang) and Libya and Egypt of the Perigondwana Realm and show close relation to the North Paleotethyan Realm, especially to the Fennosarmatian Province of southeastern Laurussia (Moesian and Scythian platforms) or to the Central Asiatic Province. A model that best fits with available evidence is that the Anatolide-Tauride Zone was either a part or located close to Laurasia in Carboniferous. The Istanbul Zone represents an equivalent of the Rhehohercynian Zone of the Central Europe and can not be compared with Intra-Alpine or south Variscan terranes which may be correlated with the Anatolide-Tauride Zone. Later, in the Permian, the Anatolide -Tauride Zone may has been separated from the Eurasian Four foraminiferal paleobiogeographic realms are distinguished in the Carboniferous - North Paleotethyan, Perigondwanian, Siberian and North American. The Carboniferous foraminiferal faunas of both the Istanbul and Anatolide-Tauride zones distinctly differ from both Cimmerian terranes (Central Afghanistan, Qiangtang) and Libya and Egypt of the Perigondwana Realm and show close relation to the North Paleotethyan Realm, especially to the Fennosarmatian Province of southeastern Laurussia (Moesian and Scythian platforms) or to the Central Asiatic Province. A model that best fits with available evidence is that the Anatolide-Tauride Zone was either a part or located close to Laurasia in Carboniferous. The Istanbul Zone represents an equivalent of the Rhehohercynian Zone of the Central Europe and can not be compared with Intra-Alpine or south Variscan terranes which may be correlated with the Anatolide-Tauride Zone. Later, in the Permian, the Anatolide -Tauride Zone may has been separated from the Eurasian
dcterms:title
Carboniferous foraminiferal paleobiogeography in Turkey and its implications for plate tectonic reconstructions Carboniferous foraminiferal paleobiogeography in Turkey and its implications for plate tectonic reconstructions Carboniferous foraminiferal paleobiogeography in Turkey and its implications for plate tectonic reconstructions
skos:prefLabel
Carboniferous foraminiferal paleobiogeography in Turkey and its implications for plate tectonic reconstructions Carboniferous foraminiferal paleobiogeography in Turkey and its implications for plate tectonic reconstructions Carboniferous foraminiferal paleobiogeography in Turkey and its implications for plate tectonic reconstructions
skos:notation
RIV/00216224:14310/03:00008139!RIV08-MSM-14310___
n3:strany
255
n3:aktivita
n17:Z n17:P
n3:aktivity
P(GA205/02/0897), Z(MSM 143100004)
n3:cisloPeriodika
2
n3:dodaniDat
n5:2008
n3:domaciTvurceVysledku
n10:6213405
n3:druhVysledku
n19:J
n3:duvernostUdaju
n11:S
n3:entitaPredkladatele
n13:predkladatel
n3:idSjednocenehoVysledku
600358
n3:idVysledku
RIV/00216224:14310/03:00008139
n3:jazykVysledku
n6:eng
n3:klicovaSlova
Istanbul Zone; Aladag Nappe; Anatolide-Tauride Zone; Laurussia
n3:klicoveSlovo
n9:Laurussia n9:Aladag%20Nappe n9:Anatolide-Tauride%20Zone n9:Istanbul%20Zone
n3:kodStatuVydavatele
IT - Italská republika
n3:kontrolniKodProRIV
[C056BA2E2C5F]
n3:nazevZdroje
Rivista Italiana di Paleontologia e Stratigrafia
n3:obor
n15:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
1
n3:projekt
n7:GA205%2F02%2F0897
n3:rokUplatneniVysledku
n5:2003
n3:svazekPeriodika
109
n3:tvurceVysledku
Kalvoda, Jiří
n3:zamer
n16:MSM%20143100004
s:issn
0035-6883
s:numberOfPages
11
n18:organizacniJednotka
14310