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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F00%3A00002603%21RIV%2F2002%2FMSM%2F143102%2FN
rdf:type
n17:Vysledek skos:Concept
dcterms:description
The Brunovistulian Terrane (BT) is a fragment of northern Gondwana margin regarded as a part of Avalonian group of terranes (KALVODA 1995). The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentation of Gondwana. It is assumed that BT was amalgamated to Baltica along the TESZ in Lower Paleozoic and during the Variscan orogeny was a southern promontory of Laurussia. The Devonian extension is assumed to be connected with intraplate stresses due to the collision of the Brunovistulian promontory with Moldanubian and Armorican Superterrane. Orogeny leads to rifting at high angle to the compression direction and rifts form first near the collision site and propagate later away from it. As a consequence, the amount of total extension and correlatively, the magnitude of the total subsidence, is commonly greatest near the suture and decreases away from it. The Moravosilesian basin bears features of both impactogen and strike-slip rela The Brunovistulian Terrane (BT) is a fragment of northern Gondwana margin regarded as a part of Avalonian group of terranes (KALVODA 1995). The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentation of Gondwana. It is assumed that BT was amalgamated to Baltica along the TESZ in Lower Paleozoic and during the Variscan orogeny was a southern promontory of Laurussia. The Devonian extension is assumed to be connected with intraplate stresses due to the collision of the Brunovistulian promontory with Moldanubian and Armorican Superterrane. Orogeny leads to rifting at high angle to the compression direction and rifts form first near the collision site and propagate later away from it. As a consequence, the amount of total extension and correlatively, the magnitude of the total subsidence, is commonly greatest near the suture and decreases away from it. The Moravosilesian basin bears features of both impactogen and strike-slip rela
dcterms:title
Paleozoic evolution of the Moravosilesian Basin Paleozoic evolution of the Moravosilesian Basin
skos:prefLabel
Paleozoic evolution of the Moravosilesian Basin Paleozoic evolution of the Moravosilesian Basin
skos:notation
RIV/00216224:14310/00:00002603!RIV/2002/MSM/143102/N
n3:strany
40
n3:aktivita
n13:P n13:Z
n3:aktivity
P(GA205/99/1640), Z(MSM 143100004)
n3:cisloPeriodika
4
n3:dodaniDat
n5:2002
n3:domaciTvurceVysledku
n18:6213405
n3:druhVysledku
n7:J
n3:duvernostUdaju
n15:S
n3:entitaPredkladatele
n16:predkladatel
n3:idSjednocenehoVysledku
721080
n3:idVysledku
RIV/00216224:14310/00:00002603
n3:jazykVysledku
n8:eng
n3:klicovaSlova
Brunovistulian terrane, extension, rifting, Devonian, Carboniferous
n3:klicoveSlovo
n4:Carboniferous n4:rifting n4:Devonian n4:extension n4:Brunovistulian%20terrane
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[D4767D537AD1]
n3:nazevZdroje
Geolines
n3:obor
n19:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
1
n3:pocetUcastnikuAkce
0
n3:pocetZahranicnichUcastnikuAkce
0
n3:projekt
n11:GA205%2F99%2F1640
n3:rokUplatneniVysledku
n5:2000
n3:svazekPeriodika
10
n3:tvurceVysledku
Kalvoda, Jiří
n3:zamer
n14:MSM%20143100004
s:issn
1210-9606
s:numberOfPages
1
n12:organizacniJednotka
14310