Zobrazeno 1 - 10
of 73
pro vyhledávání: '"Dušan, Plašienka"'
Publikováno v:
Nuclear Engineering and Technology, Vol 55, Iss 4, Pp 1485-1494 (2023)
The bow of the nuclear fuel assembly is a well-known phenomenon. One of the vital criteria during the history of nuclear fuel development has been fuel assembly’s mechanical stability. Once present, the fuel assembly bow can lead to safety issues l
Externí odkaz:
https://doaj.org/article/cd426417cacb4570a1e831be3fd694e1
Publikováno v:
Geologické práce. Správy, Vol 136, Pp 33-38 (2020)
Occurrences of magmatic rocks were identifid north of the settlement Belanskovci (part of Myjava town), on the ridge of the elevation point 464 m a. s. l. east of the settlement Podzámok (part of the Podbranč village). The volcanic rock sample was
Externí odkaz:
https://doaj.org/article/4d25d49a8b7a4ca2b29fccb2baa6b89a
Autor:
Július Vida, Pavol Gemeiner, Michaela Pavličková, Martina Mazalová, Pavel Souček, Dušan Plašienka, Tomáš Homola
Publikováno v:
Nanoscale. 15:1289-1298
We present a rapid and low-temperature (70 °C) route for the preparation of crystalline TiO2 on Ti3C2Tx MXene surfaces using atmospheric pressure oxygen plasma. Reactive oxygen species from plasma break the MXene structure and form TiO2 nanoparticle
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::57f90ed773e5b7c7add2dab9396c0fe5
https://doi.org/10.1039/d2nr04465j
https://doi.org/10.1039/d2nr04465j
Autor:
Július, Vida, Pavol, Gemeiner, Michaela, Pavličková, Martina, Mazalová, Pavel, Souček, Dušan, Plašienka, Tomáš, Homola
Publikováno v:
Nanoscale.
Composites of TiO
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::afc8f1ce60dd6529adff695c60d55a88
https://pubmed.ncbi.nlm.nih.gov/36545747
https://pubmed.ncbi.nlm.nih.gov/36545747
Autor:
Tomáš Potočný, Dušan Plašienka
The geological structure of the Western Carpathians is very complicated and is result of several deformation phases. The Meliata Unit (Meliaticum) as a significant part of the Western Carpathians proves existence of substantial tectonic movements. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e4193959707fede7de26df0df223c21b
https://doi.org/10.5194/egusphere-alpshop2022-38
https://doi.org/10.5194/egusphere-alpshop2022-38
The Lower to early Middle Jurassic terrigenous clastic deposits witness the early breakup processes of Pangaea. Rifting and subsequent ocean-floor spreading of the Central Atlantic branch that propagated eastward into the Alpine–Carpathian realm sp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::760a115e39bed19f3f06ca52859d8ef7
https://doi.org/10.5194/egusphere-alpshop2022-40
https://doi.org/10.5194/egusphere-alpshop2022-40
Publikováno v:
World Geomorphological Landscapes ISBN: 9783030892920
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d1985be159490654bb28c83d06a7f78b
https://doi.org/10.1007/978-3-030-89293-7_2
https://doi.org/10.1007/978-3-030-89293-7_2
Autor:
Dušan Plašienka, Ján Novotný
Publikováno v:
World Geomorphological Landscapes ISBN: 9783030892920
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e5e1494831995f9146f8b3426cdc0360
https://doi.org/10.1007/978-3-030-89293-7_10
https://doi.org/10.1007/978-3-030-89293-7_10
Publikováno v:
International Journal of Earth Sciences. 109:1355-1376
The Pieniny Klippen Belt (PKB) and adjoining zones form a narrow, but lengthy belt that separates the Cretaceous nappe stack of the Central (Austroalpine) and the Cenozoic accretionary wedge of the External Western Carpathians (Flysch Belt). The PKB
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44c4760f5259484d5d17d77f01fc8bf0
https://doi.org/10.1007/s00531-019-01789-5
https://doi.org/10.1007/s00531-019-01789-5
Autor:
Dušan Plašienka
Publikováno v:
Geologica Carpathica, Vol 70, Iss 1, Pp 35-61 (2019)
The paper deals with the structure and evolution of the Pieniny Klippen Belt in its classic area in western Slovakia. The so-called Peri-Klippen Zone provides a transition from the Pieniny Klippen Belt s.s. built up by Jurassic to Eocene Oravic units
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ca9743d2e67f3909a4fcaa39f6af9f5c
http://www.degruyter.com/view/j/geoca.2019.70.issue-1/geoca-2019-0003/geoca-2019-0003.xml?format=INT
http://www.degruyter.com/view/j/geoca.2019.70.issue-1/geoca-2019-0003/geoca-2019-0003.xml?format=INT