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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F13%3A10173958%21RIV14-GA0-11310___
rdf:type
skos:Concept n17:Vysledek
dcterms:description
The Teplá-Barrandian unit (TBU), occupying a central position in the Bohemian Massif, is a superbly exposed upper-crustal fragment of the Avalonian-Cadomian orogenic belt that constituted an active plate margin along the northern Gondwana during late Neoproterozoic to early Cambrian times. Despite later involved in a broad collision zone of the internal Variscan belt, the TBU, in contrast to adjacent units, largely escaped the pervasive Variscan reworking and metamorphism. In the Barrandian syncline, located between Plzeň and Prague, unmetamorphosed Cambrian to Middle Devonian successions rest unconformably on top of Neoproterozoic metasedimentary and metavolcanic rocks. Degree of regional metamorphism generally increases in the Neoproterozoic rocks from the Barrandian syncline (prehnite-pumpellyite facies at most) to the W and NW (amphibolite facies). Consequently, the TBU is a fascinating geologic archive tracing protracted, more than 300 m.y. long, tectonic history of two orogenies separated by an episode of rifting, basin development along a volcanic passive margin. During this time span, the TBU witnessed an impressive continental drift from a latitude of about 60o south at the northern margin of Gondwana in the late Neoproterozoic to its near-equator position during the final assembly of Pangea at the end of the Paleozoic Era. The GEOPilsen 2013 pre-conference field trip will take us to a selection of most instructive outcrops in the northern and northwestern TBU that record the main events of this protracted tectonic history. The Teplá-Barrandian unit (TBU), occupying a central position in the Bohemian Massif, is a superbly exposed upper-crustal fragment of the Avalonian-Cadomian orogenic belt that constituted an active plate margin along the northern Gondwana during late Neoproterozoic to early Cambrian times. Despite later involved in a broad collision zone of the internal Variscan belt, the TBU, in contrast to adjacent units, largely escaped the pervasive Variscan reworking and metamorphism. In the Barrandian syncline, located between Plzeň and Prague, unmetamorphosed Cambrian to Middle Devonian successions rest unconformably on top of Neoproterozoic metasedimentary and metavolcanic rocks. Degree of regional metamorphism generally increases in the Neoproterozoic rocks from the Barrandian syncline (prehnite-pumpellyite facies at most) to the W and NW (amphibolite facies). Consequently, the TBU is a fascinating geologic archive tracing protracted, more than 300 m.y. long, tectonic history of two orogenies separated by an episode of rifting, basin development along a volcanic passive margin. During this time span, the TBU witnessed an impressive continental drift from a latitude of about 60o south at the northern margin of Gondwana in the late Neoproterozoic to its near-equator position during the final assembly of Pangea at the end of the Paleozoic Era. The GEOPilsen 2013 pre-conference field trip will take us to a selection of most instructive outcrops in the northern and northwestern TBU that record the main events of this protracted tectonic history.
dcterms:title
From Cadomian accretion to Variscan collision: a crustal-scale traverse across the northwestern Teplá-Barrandian unit From Cadomian accretion to Variscan collision: a crustal-scale traverse across the northwestern Teplá-Barrandian unit
skos:prefLabel
From Cadomian accretion to Variscan collision: a crustal-scale traverse across the northwestern Teplá-Barrandian unit From Cadomian accretion to Variscan collision: a crustal-scale traverse across the northwestern Teplá-Barrandian unit
skos:notation
RIV/00216208:11310/13:10173958!RIV14-GA0-11310___
n17:predkladatel
n19:orjk%3A11310
n3:aktivita
n5:P n5:I
n3:aktivity
I, P(GAP210/11/1168)
n3:dodaniDat
n14:2014
n3:domaciTvurceVysledku
n8:2387689 n8:4043790 n8:8387699
n3:druhVysledku
n22:D
n3:duvernostUdaju
n11:S
n3:entitaPredkladatele
n18:predkladatel
n3:idSjednocenehoVysledku
75784
n3:idVysledku
RIV/00216208:11310/13:10173958
n3:jazykVysledku
n20:eng
n3:klicovaSlova
Variscan orogeny; Teplá-Barrandian unit; Cadomian orogeny; Bohemian Massif
n3:klicoveSlovo
n10:Tepl%C3%A1-Barrandian%20unit n10:Bohemian%20Massif n10:Variscan%20orogeny n10:Cadomian%20orogeny
n3:kontrolniKodProRIV
[87D80A7E7E61]
n3:mistoKonaniAkce
Plzeň
n3:mistoVydani
Stuttgart
n3:nazevZdroje
Crustal evolution and geodynamic processes in Central Europe. Proceedings of the Joint conference of the Czech and German geological societies held in Plzneň (Pilsen), September 1 - 19, 2013. SDGG - Schriftenreihe der Deutschen Gesselschaft für Geowissenschaften
n3:obor
n16:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
5
n3:projekt
n15:GAP210%2F11%2F1168
n3:rokUplatneniVysledku
n14:2013
n3:tvurceVysledku
Dörr, Wolfgang Hajná, Jaroslava Žák, Jiří Verner, Kryštof Zulauf, Gernold
n3:typAkce
n12:EUR
n3:zahajeniAkce
2013-09-16+02:00
s:issn
1860-1782
s:numberOfPages
30
n13:hasPublisher
Schweizerbart
n21:isbn
978-3-510-49231-2
n9:organizacniJednotka
11310