The Cambrian rocks and their tectonic evolution in the Dyminy Anticline of the Holy Cross Mts.

Authors

  • Stanisław Orłowski Institute of Geology, Warsaw University, Żwirki i Wigury 93, PL-02-089 Warszawa
  • Włodzimierz Mizerski Institute of Geology, Warsaw University, Żwirki i Wigury 93, PL-02-089 Warszawa

Abstract

The Dyminy Anticline is the Variscan tectonic unit with its core consisting of the Lower Cambrian rocks. The Cambrian core is covered by the Ordovician, Silurian and Devonian deposits on the slopes. The Lower Cambrian structure is a monocline inside which there are longitudinal tectonic grabens filled in with the Ordovician and Silurian deposits.

Downloads

Published

2013-02-22

Issue

Vol. 40 No. 3 (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).