Middle Triassic deeper-marine volcano-sedimentary successions in western Slovenia
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F25%3AND6NSGPV" target="_blank" >RIV/00216208:11320/25:ND6NSGPV - isvavai.cz</a>
Result on the web
<a href="https://www.scopus.com/inward/record.uri?eid=2-s2.0-85197943552&doi=10.5474%2fgeologija.2024.005&partnerID=40&md5=d19a79d9ca073fecef75e6e783112dd4" target="_blank" >https://www.scopus.com/inward/record.uri?eid=2-s2.0-85197943552&doi=10.5474%2fgeologija.2024.005&partnerID=40&md5=d19a79d9ca073fecef75e6e783112dd4</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5474/geologija.2024.005" target="_blank" >10.5474/geologija.2024.005</a>
Alternative languages
Result language
angličtina
Original language name
Middle Triassic deeper-marine volcano-sedimentary successions in western Slovenia
Original language description
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 Pseudozilja formation 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. © Author(s) 2024. CC Atribution 4.0 License
Czech name
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Czech description
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Classification
Type
J<sub>SC</sub> - Article in a specialist periodical, which is included in the SCOPUS database
CEP classification
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OECD FORD branch
10201 - Computer sciences, information science, bioinformathics (hardware development to be 2.2, social aspect to be 5.8)
Result continuities
Project
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Continuities
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Others
Publication year
2024
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Geologija
ISSN
0016-7789
e-ISSN
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Volume of the periodical
67
Issue of the periodical within the volume
1
Country of publishing house
US - UNITED STATES
Number of pages
33
Pages from-to
71-103
UT code for WoS article
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EID of the result in the Scopus database
2-s2.0-85197943552