Digital repository of Slovenian research organisations

Show document
A+ | A- | Help | SLO | ENG

Title:Middle Triassic deeper-marine volcano-sedimentary successions in western Slovenia
Authors:ID Skaberne, Dragomir (Author)
ID Čar, Jože (Author)
ID Pristavec, Maja (Author)
ID Rožič, Boštjan (Author)
ID Gale, Luka (Author)
Files:.pdf PDF - Presentation file, download (20,41 MB)
MD5: D1468D11E62EAB4388BAE57F71EDC2D0
 
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo GeoZS - Geological Survey of Slovenia
Abstract:A Ladinian – Carnian volcano-sedimentary succession from western Slovenia, paleogeographically belonging to the western Slovenian Basin, is presented in 17 sections. Except for the lowermost part, which is dominated by volcanics and volcaniclastics, most of the succession is dominated by shale, sandstone, and micritic limestone. Various authors use the name Pseudozilja and/or Amphiclina formation for this part, which is dominated by clastics, but they disagree on the differences between the formations. The lower Pseudozilja formation, represented by the Malenski Vrh section, comprises diabase, tuf and shale. No substantial differences in lithological composition have been observed between the upper Pseudoziljaformation and the Amphiclina formation, which are predominantly composed of shale, sandstone, and limestone. The shale and sandstone are largely composed of quartz, feldspar, and lithic grains (especially volcanics), which vary in proportions. Limestone varieties comprise hemipelagic limestones and resedimented carbonates deposited by gravity-flows. Deposition of the Ladinian – Carnian volcano-sedimentary succession took place on or near the continental slope that was generally inclined to the S, with the direction of transport mainly from N to S.
Keywords:stratigraphy, carbonate-siliciclastic deposits, Slovenian Basin, Middle Triassic, Ladinian, Carnian, Pseudozilja formation, Amphiclina formation
Publication status:Published
Publication version:Version of Record
Publication date:11.06.2024
Publisher:Geološki zavod Slovenije
Year of publishing:2024
Number of pages:str. 71-103
Numbering:vol. 67, no. 1
PID:20.500.12556/DiRROS-19208 New window
UDC:55
ISSN on article:0016-7789
DOI:10.5474/geologija.2024.005 New window
COBISS.SI-ID:198945283 New window
Publication date in DiRROS:09.07.2024
Views:305
Downloads:135
Metadata:XML DC-XML DC-RDF
:
Copy citation
  
Share:Bookmark and Share


Hover the mouse pointer over a document title to show the abstract or click on the title to get all document metadata.

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:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0011-2019
Name:Regionalna geologija

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0195-2018
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.

Secondary language

Language:Slovenian
Title:Srednjetriasna globljemorska vulkansko-sedimentna zaporedja v zahodni Slovenij
Abstract:V članku v 17 profilih predstavljamo ladinijsko – karnijsko vulkansko-sedimentno zaporedje zahodne Slovenije, paleogeografsko umeščeno v zahodni del Slovenskega bazena. Spodnji del psevdoziljske formacije, posnet na Melenskem vrhu, sestavljajo diabaz, tuf in laminiran muljevec. Zgornji del psevdoziljske formacije in amfiklinska formacija sta litološko identična. V večjem delu ju sestavljajo laminiran muljevec, peščenjak in apnenec. Glavne sestavine muljevca in peščenjaka so kremen, glinenci in litična zrna (predvsem predornin) v različnih razmerjih. Apnenec obsega hemipelagični apnenec in resedimentirane karbonate. Sedimentacija ladinijsko – karnijskega vulkansko-sedimentnega zaporedja je potekala na ali v bližini kontinentalnega pobočja z nagibom proti jugu. Transport sedimenta je v glavnem potekal od severa proti jugu.
Keywords:stratigrafija, karbonatno-siliciklastični sediment, Slovenski bazen, srednji trias, ladinij, karnij, psevdoziljska formacija, amfiklinska formacija


Collection

This document is a part of these collections:
  1. Geologija

Back