Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian unit—a correlation of U–Pb isotopic- dilution-TIMS ages (Bohemia, Czech Republic)

The Teplá–Barrandian unit (TBU) of the Bohemian Massif shared a common geological history throughout the Neoproterozoic and Cambrian with the Avalonian–Cadomian terranes. The Neoproterozoic evolution of an active plate margin in the Teplá–Barrandian is similar to Avalonian rocks in Newfoundland, w...

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Main Authors: W. Dörr A, G. Zulauf B, J. Fiala C, W. Franke A, Z. Vejnar C
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2001
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.470.6081
http://www.uni-giessen.de/fbr08/geolith/pdf-homepage/Tecton2002D%F6rr.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.470.6081 2023-05-15T17:22:35+02:00 Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian unit—a correlation of U–Pb isotopic- dilution-TIMS ages (Bohemia, Czech Republic) W. Dörr A G. Zulauf B J. Fiala C W. Franke A Z. Vejnar C The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.470.6081 http://www.uni-giessen.de/fbr08/geolith/pdf-homepage/Tecton2002D%F6rr.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.470.6081 http://www.uni-giessen.de/fbr08/geolith/pdf-homepage/Tecton2002D%F6rr.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.uni-giessen.de/fbr08/geolith/pdf-homepage/Tecton2002D%F6rr.pdf U–Pb analyses Zircons Age correlation Cadomian Orogeny Bohemian Massif text 2001 ftciteseerx 2016-01-08T07:15:45Z The Teplá–Barrandian unit (TBU) of the Bohemian Massif shared a common geological history throughout the Neoproterozoic and Cambrian with the Avalonian–Cadomian terranes. The Neoproterozoic evolution of an active plate margin in the Teplá–Barrandian is similar to Avalonian rocks in Newfoundland, whereas the Cambrian transtension and related calc-alkaline plutons are reminiscent of the Cadomian Ossa–Morena Zone and the Armorican Massif in western Europe. The Neoproterozoic evolution of the Teplá–Barrandian unit fits well with that of the Lausitz area (Saxothuringian unit), but is significantly distinct from the history of the Moravo–Silesian unit. The oldest volcanic activity in the Bohemian Massif is dated at 609+17/19 Ma (U–Pb upper intercept). Subduction-related volcanic rocks have been dated from 585F7 to 568F3 Ma (lower intercept, rhyolite boulders), which pre-dates the age of sedimentation of the Cadomian flysch (Štěchovice Group). Accretion, uplift and erosion of the volcanic arc is documented by the Neoproterozoic Dobřı́s ̌ conglomerate of the upper part of the flysch. The intrusion age of 541+7/8 Ma from the Zgorzelec granodiorite is interpreted as a minimum age of the Neoproterozoic sequence. The Neoproterozoic crust was tilted and subsequently early Cambrian intrusions dated at 522F2 Ma (Těšovice granite), 524F3 Ma (Všepadly granodiorite), 523F3 Ma (Smržovice tonalite), 523F1 Ma (Smržovice gabbro) and Text Newfoundland Unknown Morena ENVELOPE(-67.121,-67.121,-68.580,-68.580)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic U–Pb analyses
Zircons
Age correlation
Cadomian Orogeny
Bohemian Massif
spellingShingle U–Pb analyses
Zircons
Age correlation
Cadomian Orogeny
Bohemian Massif
W. Dörr A
G. Zulauf B
J. Fiala C
W. Franke A
Z. Vejnar C
Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian unit—a correlation of U–Pb isotopic- dilution-TIMS ages (Bohemia, Czech Republic)
topic_facet U–Pb analyses
Zircons
Age correlation
Cadomian Orogeny
Bohemian Massif
description The Teplá–Barrandian unit (TBU) of the Bohemian Massif shared a common geological history throughout the Neoproterozoic and Cambrian with the Avalonian–Cadomian terranes. The Neoproterozoic evolution of an active plate margin in the Teplá–Barrandian is similar to Avalonian rocks in Newfoundland, whereas the Cambrian transtension and related calc-alkaline plutons are reminiscent of the Cadomian Ossa–Morena Zone and the Armorican Massif in western Europe. The Neoproterozoic evolution of the Teplá–Barrandian unit fits well with that of the Lausitz area (Saxothuringian unit), but is significantly distinct from the history of the Moravo–Silesian unit. The oldest volcanic activity in the Bohemian Massif is dated at 609+17/19 Ma (U–Pb upper intercept). Subduction-related volcanic rocks have been dated from 585F7 to 568F3 Ma (lower intercept, rhyolite boulders), which pre-dates the age of sedimentation of the Cadomian flysch (Štěchovice Group). Accretion, uplift and erosion of the volcanic arc is documented by the Neoproterozoic Dobřı́s ̌ conglomerate of the upper part of the flysch. The intrusion age of 541+7/8 Ma from the Zgorzelec granodiorite is interpreted as a minimum age of the Neoproterozoic sequence. The Neoproterozoic crust was tilted and subsequently early Cambrian intrusions dated at 522F2 Ma (Těšovice granite), 524F3 Ma (Všepadly granodiorite), 523F3 Ma (Smržovice tonalite), 523F1 Ma (Smržovice gabbro) and
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author W. Dörr A
G. Zulauf B
J. Fiala C
W. Franke A
Z. Vejnar C
author_facet W. Dörr A
G. Zulauf B
J. Fiala C
W. Franke A
Z. Vejnar C
author_sort W. Dörr A
title Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian unit—a correlation of U–Pb isotopic- dilution-TIMS ages (Bohemia, Czech Republic)
title_short Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian unit—a correlation of U–Pb isotopic- dilution-TIMS ages (Bohemia, Czech Republic)
title_full Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian unit—a correlation of U–Pb isotopic- dilution-TIMS ages (Bohemia, Czech Republic)
title_fullStr Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian unit—a correlation of U–Pb isotopic- dilution-TIMS ages (Bohemia, Czech Republic)
title_full_unstemmed Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian unit—a correlation of U–Pb isotopic- dilution-TIMS ages (Bohemia, Czech Republic)
title_sort neoproterozoic to early cambrian history of an active plate margin in the teplá–barrandian unit—a correlation of u–pb isotopic- dilution-tims ages (bohemia, czech republic)
publishDate 2001
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.470.6081
http://www.uni-giessen.de/fbr08/geolith/pdf-homepage/Tecton2002D%F6rr.pdf
long_lat ENVELOPE(-67.121,-67.121,-68.580,-68.580)
geographic Morena
geographic_facet Morena
genre Newfoundland
genre_facet Newfoundland
op_source http://www.uni-giessen.de/fbr08/geolith/pdf-homepage/Tecton2002D%F6rr.pdf
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http://www.uni-giessen.de/fbr08/geolith/pdf-homepage/Tecton2002D%F6rr.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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