Tectonic style of the Early Palaeozoic sequences in the Holy Cross Mountains

Authors

  • Jerzy Znosko Polish Geological Institute, Rakowiecka 4, PL-00-975 Warszawa

Abstract

Thirty two localities (outcrops and boreholes) have been described and analyzed from the structural point of view. The evidence is given that the structural style of folds, imbrications and overthrusts is similar in the both Early Palaeozoic units; southern (Dyminy-Klimontów) and northern (Łysogóry). A new overthrust (Bronkowice-Zawichost-Biłgoraj) has been indicated in the north. Holy Cross Fault is a result of thrusting of the Łysogóry Range over the Devonian of the Kielce-Łagów Synclinorium in the syn-Variscan syn-Alpine epochs.

Downloads

Published

2013-02-13

Issue

Vol. 40 No. 1 (1996)

Section

Articles

License

Authors who publish with this journal agree to the following terms:
  1. Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
  2. Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
  3. Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as this can lead to productive exchanges and earlier and more frequent citation of the published work (See The Effect of Open Access).