Zobrazeno 1 - 10
of 15
pro vyhledávání: '"krško basin"'
Publikováno v:
Geologija, Vol 64, Iss 1, Pp 5-19 (2021)
It has been supposed that the Brežice Sava River Terrace (BSRT) is tectonically disturbed near the town of Brežice and tilted to the north. To confirm this tectonically induced tilt in a quantitative sense, low-frequency Ground Penetration Radar
Externí odkaz:
https://doaj.org/article/c6596ec1be5141538d90559b604d0ac4
Publikováno v:
CAAI Transactions on Intelligence Technology (2019)
This study describes an application of hybrid modelling for an atmospheric variable in the Krško basin. The hybrid model is a combination of a physics-based and data-driven model and has some properties of both modelling approaches. In the authors
Externí odkaz:
https://doaj.org/article/28e0ff71274945669404dba8c21424c2
Publikováno v:
CAAI Transactions on Intelligence Technology (2019)
This study describes an application of hybrid modelling for an atmospheric variable in the Krško basin. The hybrid model is a combination of a physics-based and data-driven model and has some properties of both modelling approaches. In the authors
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a585e5c2225f5daa59bdd2694babb1c9
https://doi.org/10.1049/trit.2019.0054
https://doi.org/10.1049/trit.2019.0054
Publikováno v:
Geologija, Vol 48, Iss 1, Pp 23-32 (2005)
Based on seismic reflection profiles recorded in the last ten years in the frame of the investigations for assessment of earthquake hazard at the location of the Krško nuclear power plant, and taking into account relevant geological and gravimetric
Externí odkaz:
https://doaj.org/article/4c70b1f734574f19a8bd0aedcf8aabfe
Autor:
Aleksander Horvat
Publikováno v:
Geologija, Vol 46, Iss 2, Pp 251-262 (2003)
In the western part of Central Paratethys, on the territory of Slovenia, the Upper Badenian diatoms occur only in the Kr{ko basin. The diatom paleoecology of the Upper Badenian beds suggests their deposition in the marine littoral, in warm to moderat
Externí odkaz:
https://doaj.org/article/a7ba6adbc7b54bf9900b47337ded45a3
Autor:
Marinšek, Miha
Namen magistrske naloge je bila določitev ostrakodne zdužbe, paleookolja in starosti Bizeljske formacije v Krški kotlini. V ta namen je bil raziskan 43 metrov debel odsek formacije na območju Bizeljskega. Ostrakodi Bizeljske formacije pripadajo d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3505::81f5b5786ea99a9dd9e9f419a1119778
https://repozitorij.uni-lj.si/Dokument.php?id=133942&dn=
https://repozitorij.uni-lj.si/Dokument.php?id=133942&dn=
Autor:
Sršen, Saša
V magistrskem delu prikažejo uporabo dendrokronologije kot arheološke naravoslovne metode za razumevanje klime v preteklosti. Za potrebe rekonstrukcije klime je bilo potrebno vzorčenje živih dreves in vgrajenega lesa v Krški kotlini in na Lonjsk
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3505::87669a605879d78557df15d420997f82
https://repozitorij.uni-lj.si/IzpisGradiva.php?id=112918
https://repozitorij.uni-lj.si/IzpisGradiva.php?id=112918
Publikováno v:
Geologija, Vol 48, Iss 1, Pp 23-32 (2005)
Based on seismic reflection profiles recorded in the last ten years in the frame of the investigations for assessment of earthquake hazard at the location of the Krško nuclear power plant, and taking into account relevant geological and gravimetric
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89b5174403e4eab8269113148a96c1f0
https://doi.org/10.5474/geologija.2005.004
https://doi.org/10.5474/geologija.2005.004
Krško basin in southern Slovenia is historically, as well as prehistorically seismically active region. Geotectonically, it is situated at the western rim of the Pannonian basin and represents southern part of Sava folds which were formed as a resul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::8ff3d2721aac09f2f0a9f41964db46b4
https://www.bib.irb.hr/180051
https://www.bib.irb.hr/180051
Autor:
Marjanac, Ljerka, Marjanac, Tihomir
Seismogenic sediment deformation structures, namely seismites have been recognized in 3 intervals of Raka sand deposits and Globoko sand interval of the Pontian age. There were 8 types of small-scale seismogenic deformations distinguished in the Raka
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::fcaae931422688b8a0134e51a7a2fb12
https://www.bib.irb.hr/32723
https://www.bib.irb.hr/32723