Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Viera Šimonová"'
Stratiform U-Cu mineralization (0.02-1.13 % U) in the eastern part of the Kozie Chrbty Mts. is bound to the Permian volcano-sedimentary complex of the Ipoltica Group, Hronic Unit (Western Carpathians). The wide surroundings of the deposits are formed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d2873f073406c96f2ad35e80c97ceec3
https://doi.org/10.5194/egusphere-alpshop2022-53
https://doi.org/10.5194/egusphere-alpshop2022-53
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
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
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
Publikováno v:
Geologica Carpathica, Vol 69, Iss 4, Pp 365-381 (2018)
The Manín Unit represents a transitional tectonic element between the Central Western Carpathians and the Pieniny Klippen Belt. The overall map-view structure of the Manín Unit is dominated by elliptical antiforms composed of comparatively competen
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
Publikováno v:
Geologica Carpathica, Vol 68, Iss 5, Pp 403-418 (2017)
The Súľov Conglomerates represent mass-transport deposits of the Súľov-Domaniža Basin. Their lithosomes are intercalated by claystones of late Thanetian (Zones P3 - P4), early Ypresian (Zones P5 - E2) and late Ypresian to early Lutetian (Zones E
Publikováno v:
Journal of Geosciences. :239-254
Autor:
Viera Šimonová, Dušan Plašienka
Publikováno v:
Geological Quarterly. 61
This study aims at quantitative kinematic analysis of fault-slip data and palaeostress reconstruction of polyphase brittle structures developed in the Manin Unit cropping out in the Middle Vah River Valley of western Slovakia. The Manin Unit neighbou
Publikováno v:
Scopus-Elsevier
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::292c545648de114be4488dd92f111f8c
http://www.scopus.com/inward/record.url?eid=2-s2.0-85070441371&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-85070441371&partnerID=MN8TOARS