Palaeogeography of the uppermost Carboniferous and lowermost Permian deposits in the NE part

Authors

  • Andrzej Bossowski xxx
  • Adam Ihnatowicz xxx

Abstract

of the Intra-Sudetic Depression Based on analysis of sediments of the uppermost palaeogeography and the lowermost Permian, the fundamental palaeogeography of the Intra-Sudetic Depression has been reconstructed at the boundary of tile Westphalian and Stephanian (the Asturian phase). Main source areas in the upper Westphalian occurred south of Wałbrzych and west of Nowa Ruda. The Wałbrzych region and the present area of the Góry Sowie Block were the source areas of the coarse-grained material, sedimentation being development mainly near the present Polish-Czech border and on the Czech side of the Intra-Sudetic Depression. River deposition, dominant in the uppermost Carboniferous, gradually changed to lacustrine deposition.

Downloads

Published

2013-02-25

Issue

Vol. 38 No. 4 (1994)

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).