Zagadnienia sedymentacji utworów fliszowych pienińskiego pasa skałkowego Polski

Authors

  • Krzysztof Birkenmajer

Abstract

SEDIMENTOLOGICAL PROBLEMS OF THE FLYSCH DEPOSITS OF THE PIENINY KLIPPEN BELT OF POLANDIn the Pieniny Klippen Belt of Poland the flysch deposits of the Aalenian, Senonian, and Palaeogene ages have been found. The flysch deposits of the Aalenian (Flysch Aalenian) are up to 200 m thick. It is believed· that the clastic material of the Flysch Aalenian derived from the Upper Carboniferous deposits which emerged in connection with the Mid-Cimmerian synorogenic movements on so-called Central Cordilliera, withm the basin of the Klippen Series.For the second time the flysch deposits appeared, in the Pieniny Klippen Belt of Poland, at the Lower Senionan time. This is a pre-orogenic flysch represented by the Sromowce Beds, some 100 m thick. The source area of the flysch deposits was situated south of the basin of the Klippen Series.

Downloads

Issue

Vol. 7 No. 2 (1963)

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).