Kierunki transportu materiału klastycznego w górnym karbonie Górnośląskiego Zagłębia Węglowego
Abstract
DIRECTIONS OF TRANSPORT OF THE CLASTIC MATERIAL IN THE UPPER CARBONIFEROUS OF THE SILESIAN COAL BASINThe Upper Carboniferous sandstones of the Silesian Coal Basin are very often cross-bedded. Both torrential and tangential types of cross-bedding are present, and each of them is·represented by a number of varieties. Following the terminology of McKee and Weir (1953) the authors distinguished the parallel torrential cross-stratification (ng. 1) and wedge-shaped torrential cross-stratification (Fig. 2). Parallel, wedge-shaped and trough cross-stratification varieties were distinguished within the tangential type of cross-stratification (Fig. 3, Fig. 4 and Fig. 5). The term “irregular current beddingˮ was, proposed by the authors (B. Gradziński, A. Radomski, R. Unrug 1959) for irregular current-bedded streaks occurring, within beds of fine-grained sandstones. This type of current bedding is also common in the Silesian Upper Carboniferous.Downloads
Issue
Section
Articles
License
Authors who publish with this journal agree to the following terms:- 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.
- 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.
- 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).