Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Juraj Butek"'
Publikováno v:
Minerals, Vol 12, Iss 2, p 195 (2022)
Ostrá Lúka basalts are a product of the final phase of Neogene volcanism in Central Slovakia. Their major and trace elements composition is alkaline, a feature confirmed by light rare earth elements (LREE) relative enrichment and some incompatible
Externí odkaz:
https://doaj.org/article/856c9a4110d24cadba7f9ec035c66d1b
Publikováno v:
Minerals, Vol 11, Iss 8, p 841 (2021)
The paper presents new geochemical data of the basic to intermediate volcanic rocks from the Hronic unit. The studied rocks are strongly altered and the primary mineral composition (clinopyroxenes, amphiboles, spinels, biotites, and plagioclases) is
Externí odkaz:
https://doaj.org/article/1318f9aa4847427084887a489f8e86db
Publikováno v:
Minerals, Vol 11, Iss 2, p 189 (2021)
Intensively metasomatized rocks from serpentinized ultramafic tectonic fragments in Dobšiná, Western Carpathians, consist of typical rodingite mineral association: hydrated garnet, vesuvianite, diopside and clinochlore. Electron microprobe analysis
Externí odkaz:
https://doaj.org/article/12d315e5276049358bd0089e552f4609
Autor:
David Chew, Tomáš Mikuš, Viera Šimonová, Štefan Ferenc, Lucia Vetráková, Juraj Butek, Ján Spišiak
Publikováno v:
Geological Society, London, Special Publications. 513:297-321
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8976f45640864f474a5e42a81a05906e
https://doi.org/10.1144/sp513-2020-237
https://doi.org/10.1144/sp513-2020-237
Publikováno v:
Minerals; Volume 12; Issue 2; Pages: 195
Ostrá Lúka basalts are a product of the final phase of Neogene volcanism in Central Slovakia. Their major and trace elements composition is alkaline, a feature confirmed by light rare earth elements (LREE) relative enrichment and some incompatible
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=multidiscipl::fa6e599e56b886217c219421dfcc9bc1
Publikováno v:
Lithos
Lithos, 2022, 432-433, pp.106902. ⟨10.1016/j.lithos.2022.106902⟩
Lithos, 2022, 432-433, pp.106902. ⟨10.1016/j.lithos.2022.106902⟩
International audience; Rodingite represents a particular metasomatic rock type that occurs as dykes or lenses in association with serpentinized ultramafic rocks and typically consists of Ca-rich, often hydrated silicate minerals. Rodingites have bee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::877850868bf10f6ab88f9a0c79c2ebea
https://hal.science/hal-03836730
https://hal.science/hal-03836730
Publikováno v:
Minerals, Vol 11, Iss 189, p 189 (2021)
Minerals
Volume 11
Issue 2
Minerals
Volume 11
Issue 2
Intensively metasomatized rocks from serpentinized ultramafic tectonic fragments in Dobšiná, Western Carpathians, consist of typical rodingite mineral association: hydrated garnet, vesuvianite, diopside and clinochlore. Electron microprobe analysis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d9f6bb4cd0394df57d3017b87e57b024
https://www.mdpi.com/2075-163X/11/2/189
https://www.mdpi.com/2075-163X/11/2/189
Publikováno v:
Minerals. 12:195
Ostrá Lúka basalts are a product of the final phase of Neogene volcanism in Central Slovakia. Their major and trace elements composition is alkaline, a feature confirmed by light rare earth elements (LREE) relative enrichment and some incompatible
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bbe675ecd02b8c866c42e80bde5ee5bb
https://doi.org/10.3390/min12020195
https://doi.org/10.3390/min12020195
Publikováno v:
Minerals, Vol 11, Iss 841, p 841 (2021)
Minerals
Volume 11
Issue 8
Minerals
Volume 11
Issue 8
The paper presents new geochemical data of the basic to intermediate volcanic rocks from the Hronic unit. The studied rocks are strongly altered and the primary mineral composition (clinopyroxenes, amphiboles, spinels, biotites, and plagioclases) is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7ec08fb1b67f9f859eb24b079295c713
https://doi.org/10.3390/min11080841
https://doi.org/10.3390/min11080841