Budowa geologiczna pogranicza synklinorium szczecińskiego z antyklinorium pomorskim w okolicy Zalewu Szczecińskiego
Abstract
GEOLOGICAL STRUCTURE OF THE AREA SITUATED BETWEEN THE SZCZECIN SYNCLINORIUM AND POMERANIAN ANTICLINORIUM IN THE VICINITY OF SZCZECIN LAGOONSummaryOn the basis of reflection seismics and on the results of few bore holes the tectonics of the area situated immediately east of the Dziwna River and of the Wolin and Uznam islands is presented. To the main structural elements of this tectonics belong here: Lubin anticline, Międzyzdroje anticline, Dargobądz anticline, Wisełka syncline, Recław anticline and Strzegów syncline. Phenomena of salt tectonics have not been ascertained here.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).