Zobrazeno 1 - 10
of 75
pro vyhledávání: '"Kryštof Verner"'
Autor:
Jaroslava Pertoldová, Kryštof Verner, David Buriánek, Jan Valenta, Barbora Dudíková, Zuzana Skácelová, Jan Jelének, Jan Jelínek, Kenneth Johnson, Otmar Petyniak, Petra Hejtmánková
Publikováno v:
Journal of Maps, Vol 20, Iss 1 (2024)
ABSTRACTThe geological map of the Klenov Pluton (Moldanubian Batholith), and its 3D visualization, brings the new findings in the context of granite emplacement within late-Variscan settings. The Klenov Pluton has a peraluminous composition resulting
Externí odkaz:
https://doaj.org/article/56bd955eda494e76a24a501220ea1b84
Autor:
Wanru Li, Mekuanent Muluneh Finsa, Kathryn Blackmond Laskey, Paul Houser, Rupert Douglas-Bate, Kryštof Verner
Publikováno v:
Water, Vol 16, Iss 19, p 2715 (2024)
Utilizing groundwater offers a promising solution to alleviate water stress in Ethiopia, providing a dependable and sustainable water source, particularly in regions with limited or unreliable surface water availability. However, effective decision-m
Externí odkaz:
https://doaj.org/article/2fcde5ed75f642ba8d0fd91c75c31287
Publikováno v:
Quaternary International. 656:1-15
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c50ceb4705660828b09049f1874238d1
https://doi.org/10.1016/j.quaint.2023.01.008
https://doi.org/10.1016/j.quaint.2023.01.008
Autor:
Leta Megerssa, Kryštof Verner, David Buriánek, Ondřej Pour, Filip Tomek, David Schiller, Karel Martínek
Publikováno v:
International Journal of Earth Sciences. 112:631-658
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa7cbd77317dadd4313949ef4e89e8b9
https://doi.org/10.1007/s00531-022-02258-2
https://doi.org/10.1007/s00531-022-02258-2
Autor:
Fritz Finger, David Schiller, Martin Lindner, Christoph Hauzenberger, Kryštof Verner, Jiří Žák
Publikováno v:
Geology. 50:542-546
Comprehensive zircon thermometry that takes into account zircon saturation temperatures, Ti-in-zircon measurements, and zircon morphologies and microstructures can provide key information on the thermal evolution of a granite batholith. The Variscan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b35ca6faaf649393725f162ac9d5589e
https://doi.org/10.1130/g49645.1
https://doi.org/10.1130/g49645.1
Autor:
Kryštof Verner, Ferdawok Legesse, Meheret Yakob, Jan Boháč, Jan Valenta, Muluken Kassa, Bisrat Kebede, Jiří Málek, Tomáš Hroch, Leta Megerssa, David Buriánek, Karel Martínek
Publikováno v:
Earth Surface Processes and Landforms. 46:3158-3174
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7489794f47dae701cc1e93678aff6680
https://doi.org/10.1002/esp.5227
https://doi.org/10.1002/esp.5227
Publikováno v:
Geosciences, Vol 9, Iss 3, p 104 (2019)
A composite lamprophyre dyke from the Central Bohemian Dyke Swarm (Czech Republic) shows both indications of magma free flow (normal magnetic fabric with magnetic foliation and lineation parallel to the dyke plane) as well as those of forcefully driv
Externí odkaz:
https://doaj.org/article/575335b1f01e4686a3c6d99abf7ea58a
Autor:
Martin Svojtka, Axel Gerdes, J. Stephen Daly, Kristýna Hrdličková, Petr Gadas, Vojtěch Janoušek, František V. Holub, Pavel Hanžl, John M. Hora, David Buriánek, Yulia V. Erban Kochergina, Kryštof Verner
Publikováno v:
International Journal of Earth Sciences. 109:1767-1810
The Třebic Pluton (TP) comprises plutonic rocks of the ‘durbachite series’, i.e., ultrapotassic biotite–amphibole quartz melasyenites–melagranites with conspicuous K-feldspar phenocrysts and abundant mafic enclaves. The TP with its satellite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bea5eea420dab996e6f0efa494945898
https://doi.org/10.1007/s00531-020-01872-2
https://doi.org/10.1007/s00531-020-01872-2
Autor:
Vojtěch Janoušek, Axel Gerdes, Shane Tyrrell, Renata Čopjaková, František V. Holub, Jan Košler, Kryštof Verner, John M. Hora
Publikováno v:
Lithos. :239-262
In the Variscan Bohemian Massif, (ultra-)potassic plutons are conspicuously associated with the high-grade, lower crustal/upper mantle Gfohl Unit (Moldanubian Zone). They can be subdivided into two contrasting groups: (1) coarse amphibole–biotite m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72443e04abbb05a403697189c543afd5
https://doi.org/10.1016/j.lithos.2019.05.028
https://doi.org/10.1016/j.lithos.2019.05.028
Publikováno v:
Tectonophysics. 766:379-397
An extensive early Carboniferous foreland basin (the Moravosilesian Culm Basin, MSCB) delineates the northeastern margin of the Bohemian Massif (Variscan orogenic belt). The basin overlays a complex suture between the outer Brunovistulia microplate,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f10ddfeb5768dfeb135a8279e588ae4
https://doi.org/10.1016/j.tecto.2019.05.023
https://doi.org/10.1016/j.tecto.2019.05.023