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Title:Upper Triassic–to Lower Cretaceous Slovenian Basin successions in the northern margin of the Sava Folds
Authors:ID Scherman, Benjamin (Author)
ID Rožič, Boštjan (Author)
ID Görög, Ágnes (Author)
ID Kövér, Szilvia (Author)
ID Fodor, László (Author)
Files:.pdf PDF - Presentation file, download (27,89 MB)
MD5: 7307AA535E95E1721224EBFE904CBD58
 
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo GeoZS - Geological Survey of Slovenia
Abstract:The evolution of the Slovenian Basin southern margin is currently interpreted based on the successions outcropping in the surroundings of Škofja Loka, on the Ponikve Plateau and in the foothills of the Julian Alps in western Slovenia, as well as from the valley of the Mirna River in south-eastern Slovenia. However, no extensive research on this paleogeographic unit has been carried out in the northern part of the Sava Folds region. Recent field observations permitted the recognition of Upper Triassic to lowermost Cretaceous successions of the Slovenian Basin, including the recently described Middle Jurassic Ponikve Breccia Member of the Tolmin Formation. Based on reambulation-type geological mapping, macroscopic facies observations supported by microfacies analysis and biostratigraphy, three stratigraphic columns were constructed showcasing Slovenian Basin formations on the northern flank of the Trojane Anticline (Sava Folds region). These newly described successions encompass Upper Triassic (Bača Dolomite Formation) and Jurassic–lowermost Cretaceous resedimented limestones and pelagic formations, while the attribution of the Pseudozilian Formation is complex. Based on facies characteristics these successions are similar to those preserved in the Podmelec Nappe (lowermost thrust unit of the Tolmin Nappe) in western Slovenia. The connection between the western and the eastern Slovenian Basin during the Late Triassic-Early Cretaceous interval could be thus recognised.
Keywords:Southern Alps, Sava Folds, Slovenian Basin, Jurassic, Ponikve Breccia, stratigraphy, foraminifera
Publication status:Published
Publication version:Version of Record
Publication date:21.12.2023
Publisher:Geološki zavod Slovenije
Year of publishing:2023
Number of pages:str. 205-228
Numbering:vol. 66, no. 2
PID:20.500.12556/DiRROS-17798 New window
UDC:551.7
ISSN on article:0016-7789
DOI:10.5474/geologija.2023.009 New window
COBISS.SI-ID:179224067 New window
Publication date in DiRROS:15.01.2024
Views:213
Downloads:131
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Record is a part of a journal

Title:Geologija
Shortened title:Geologija
Publisher:Geološki zavod Slovenije
ISSN:0016-7789
COBISS.SI-ID:5636866 New window

Document is financed by a project

Funder:Other - Other funder or multiple funders
Funding programme:National Research, Development and Innovation Office of Hungary
Project number:No. 134873
Acronym:NKFIH OTKA

Funder:ARRS - Slovenian Research Agency
Project number:P1-0195
Name:Geookolje in geomateriali

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.
Licensing start date:21.12.2023

Secondary language

Language:Slovenian
Title:Zgornjetriasno do spodnjekredno zaporedje Slovenskega bazena iz severnega roba Posavskih gub
Abstract:Razvoj južnega obrobja Slovenskega bazena je trenutno poznan na podlagi zaporedij, ki izdanjajo v okolici okrog Škofje Loke, na Ponikvanski planoti in iz predgorja Julijskih Alp v zahodni Sloveniji ter iz doline reke Mirne v jugovzhodni Sloveniji. Nasprotno do sedaj še ni bilo celostne stratigrafske študije globljemorskih zaporedij iz severnega dela Posavskih gub. Tekom nedavnih terenskih raziskav smo na tem območju prepoznali zgornjetriasno do spodnje kredno zaporedje Slovenskega bazena, ki vsebuje tudi nedavno opisan člen Ponikvanske breče Tolminske formacije. Na podlagi reambulacijskega geološkega kartiranja, makroskopskega opazovanja faciesov, katerega smo podprli z mikroskopsko analizo in biostratigrafijo, smo izdelali tri stratigrafske stolpce, ki prikazujejo zaporedje Slovenskega bazena vzdolž severnih obronkov Posavskih gub (Trojanske antiklinale). Novo prepoznano zaporedje vključuje zgornjetriasni Baški dolomit in jurske do spodnjekredne presedimentirane apnence in pelagične sedimente. Faciesne značilnosti kažejo, da ta del Posavskih gub pripada vzhodno nadaljevanje Podmelškega pokrova (spodnje podenote Tolminskega pokrova). S tem je prepoznana povezava med zahodnimi in vzhodnimi zaporedji Slovenskega bazena.
Keywords:Južne Alpe, Posavske gube, Slovenski bazen, Ponikvanska breča, stratigrafija, foraminifere


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  1. Geologija

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