O kulmie z okolic Toszka

Authors

  • Antoni Marian Żelichowski

Abstract

ON THE CULM FROM THE REGION OF TOSZEKThe region discussed by the author is situated in the NW periphery of the Cracow-Silesia-Karvina Coal Basin. From under a mantle of younger sediments - Triassic, Tertiary and Quaternary - there emerge in the Toszek region greywacke sandstones and shales. Since long they have been looked upon as Lower Carboniferous sediments. It was impossible to identify accurately the age of the fauna found there; however, on the basis of sediments containing an analogous fauna and of tectonic data, these sediments were assigned to the highest part of the Lower Carboniferous, i.e. the highermost Visean (horizon Goniatites granosus).

Downloads

Issue

Vol. 6 No. 2 (1962)

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).