The ‘microcontinent’ Perunica: status and story 15 years after conception-Reference-Cited by-同舟云学术

The ‘microcontinent’ Perunica: status and story 15 years after conception

Published:2009 Issue:1 Volume:325 Page:65-101
ISSN:0305-8719
Container-title:Geological Society, London, Special Publications
language:en
Short-container-title:Geological Society, London, Special Publications

Author:

Fatka Oldřich¹,Mergl Michal²

Affiliation:

1. Institute of Geology and Palaeontology, Faculty of Science, Charles University, Albertov 6, Prague 2, 128 43, Czech Republic

2. Department of Biology, University of West Bohemia, Klatovská 51, 306 19, Plzeň, Czech Republic

Abstract

AbstractCentral Europe consists of a complex mosaic of more or less independent terranes with varying tectonometamorphic histories, usually also of different lithological compositions and protolith, and thus it is reasonable to suppose that the majority of these blocks have experienced somewhat different palaeogeographical evolution. The present terrane juxtaposition has been interpreted in general as a result of the Variscan collision of peri-Gondwanan and peri-Baltic derived terranes, with Gondwana on one side and Baltica and/or Laurentia on the other side. However, reconstruction of the pre-Variscan development and mutual palaeogeographical relationships remains a major challenge of interpretation.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

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