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)

• 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: U–Pb analyses; Zircons; Age correlation; Cadomian Orogeny; Bohemian Massif; Morena; Newfoundland
• 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

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...