Zobrazeno 1 - 10
of 30
pro vyhledávání: '"Tomislav Popit"'
Autor:
Boštjan Rožič, Anja Kocjančič, Luka Gale, Nina Zupančič, Tomislav Popit, Primož Vodnik, Tea Kolar-Jurkovšek, Rok Brajkovič, Petra Žvab Rožič
Publikováno v:
Swiss Journal of Geosciences, Vol 117, Iss 1, Pp 1-24 (2024)
Abstract The study area is located in cental Slovenia, and geologically located at the junction between the Alps and the Dinarides. The Middle Triassic of this region is characterised by intense rifting manifested by differential subsidence and volca
Externí odkaz:
https://doaj.org/article/becc46b5d7c249a0946a84d8267d26e4
Autor:
Boštjan Rožič, Luka Gale, Primož Oprčkal, Astrid Švara, Tomislav Popit, Lara Kunst, Dragica Turnšek, Tea Kolar-Jurkovšek, Andrej Šmuc, Aljaž Ivekovič, Jan Udovč, David Gerčar
Publikováno v:
Geologija, Vol 65, Iss 2, Pp 177-216 (2022)
In the southernmost outcrops of the Slovenian Basin the Middle Jurassic coarse-grained limestone breccia (mega)beds are interstratified within a succession that is otherwise dominated by hemipelagites and distal turbidites. In this paper, these beds
Externí odkaz:
https://doaj.org/article/520135cadcc14a6a9aa5755350941718
Publikováno v:
Remote Sensing, Vol 14, Iss 9, p 2016 (2022)
The northern slopes of the Vipava Valley are defined by a thrust front of Mesozoic carbonates over Tertiary flysch deposits. These slopes are characterized by a variety of different surface forms, among which recent and fossil polygenetic landslides
Externí odkaz:
https://doaj.org/article/2c5d1de1e4d249c199c31d607299512f
Publikováno v:
Journal of Maps, Vol 14, Iss 2, Pp 382-391 (2018)
We present a geomorphological map on a scale of 1:15,000, with detailed sedimentological descriptions, and a general relative spatio-temporal depositional reconstruction of Quaternary sediments in the Planica-Tamar Valley (NW Slovenia). After the Las
Externí odkaz:
https://doaj.org/article/9f8c197622ad47d5b8e280f30c4c02e2
Autor:
Bostjan Rožič, Tomislav Popit, Luka Gale, Timotej Verbovšek, Ines Vidmar, Matej Dolenec, Petra Žvab Rožič
Publikováno v:
Acta Carsologica, Vol 48, Iss 3 (2019)
The Julian Alps are composed almost exclusively of Triassic to Lower Jurassic carbonates, which results in a karstified high-alpine landscape. In such settings, large water accumulations are not expected and precipitated water drains vertically, ga
Externí odkaz:
https://doaj.org/article/9a6d38c68b674ba887162f2f91864721
Autor:
Tomislav Popit
Publikováno v:
Geologija, Vol 60, Iss 2, Pp 297-307 (2017)
The Rebrnice area forms the north eastern slopes of the Upper Vipava Valley and is located between Karst plateau to the southwest and the Nanos plateau to the northeast. The Rebrnice slopes are geomorphologically defied by a thrust front of Mesozoi
Externí odkaz:
https://doaj.org/article/9dd88653fed543b48d1e146ce38879d3
Publikováno v:
Geologija, Vol 60, Iss 1, Pp 145-155 (2017)
The Rebrnice area in the Upper Vipava Valley, SW Slovenia, is covered by Quaternary slope deposits that are very complex in their genesis and composition. Some of the sediments are deposited in the form of heterogeneously composed fossil landslides
Externí odkaz:
https://doaj.org/article/34c484d49a2944f1bd150427762c0229
Publikováno v:
Acta Geographica Slovenica, Vol 59, Iss 1, Pp 7–22-7–22 (2019)
The area of Lokavec in the Vipava Valley, SW Slovenia, consists of Mesozoic carbonates thrust over Paleogene siliciclastic flysch. Overthrusting and tectonic damage of carbonates accelerated their mechanical disintegration. As a result, accumulations
Externí odkaz:
https://doaj.org/article/9387fb27e3c0454487c3d15284f7038d
Publikováno v:
Geodetski Vestnik, Vol 60, Iss 2, Pp 227-240 (2016)
A method that gives the clearest individual geomorphometric elements for the requirements of spatial analysis was selected to define the spatial variability of landforms on primary bedrocks and their slope deposits on the northern edge of the Vipava
Externí odkaz:
https://doaj.org/article/92315268211f4c6393197346cce97ba8
Autor:
Boštjan Rožič, Tomislav Popit
Publikováno v:
Geologija, Vol 49, Iss 2, Pp 219-234 (2006)
The Middle and Upper Jurassic succession of the Slovenian Basin is characterized by pelagic sedimentation of siliceous limestones and radiolarian cherts. In the southern and central part of the basin two packages of resedimented limestones are interb
Externí odkaz:
https://doaj.org/article/9305eb24179543048d586f4cb9496bda