Dolny karbon w okolicy Łagowa
Abstract
THE LOWER CARBONIFEROUS IN THE ŁAGÓW REGION (ŚWIĘTY KRZYŻ MOUNTAINS)The Lower Carboniferous of the region of Łagów lies in the central part of the Święty Krzyż Mountains. The exposures west of Łagów represent the youngest deposits of the Łagów syncline, whereas the Lower Carboniferous situated east of Łagów belongs to the Sobiekurów - Piotrrów basin (Fig. 1). The furmer exposures have been investigated by J. Czarnocki (1922, 1924, 1928, 1929) who reported for them diagrammatically their lithological and stratigraphical section without, however, defining their index fauna. The Lower Carboniferous which occurs east of Łagów has so far been one of the least investigated areas of the Święty Krzyż Mountains; in geological literature this area has been mentioned, but without details (J. Samsonowicz, 1900, 1934).In 1957, 11006, and partly 1959 too, I have been doing field work in this region (shallow diggings, deeper test holes, exploratory trenches), finding fossils, among them index goniatites; I also determined the extent of these sediments.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).