Some problems of a geodynamic model of the Northern Carpathian
Abstract
Modified picture of the Earth's crust structure in the Northern Carpathians and their foreland (Fig. 1) is discussed. Karlovy Vary - Radom - Chernigov deep fracture is implied, being introduced as a northern boundary of the Meta-Carpathian range. This fracture cuts both Paleozoic and pre-Vendian (East European) platforms as far as Dnepr-Donetz aulacogen (Fig. 2). According to author's new analysis the western extremity of the Skole flysch near Brzesko is connected with the southern extension of western slope of the Mid-Polish aulacogen. Since Campanian mobile San massif (southern part of the Mid-Polish anticlinorium) was a source area for submarine slumpings and olistolites in the Skole flysch of Przemyśl region. Thrust directions of the Carpathian flysch masses are discussed.Downloads
Published
2013-05-07
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).