Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Jan Franěk"'
Publikováno v:
Geoscience Research Reports. :17-20
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6177d2c8c7a7969d636f14d496e88e2
https://doi.org/10.3140/zpravy.geol.2019.03
https://doi.org/10.3140/zpravy.geol.2019.03
Magnetostatic susceptibility of single crystals of graphite is negative (the mineral is diamagnetic) and strongly anisotropic. The in-phase component of dynamic susceptibility (measured in alternating magnetic field) is also negative, but an order-of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8414b6b3748f12c9a86075f264133db0
https://doi.org/10.5194/egusphere-egu21-2385
https://doi.org/10.5194/egusphere-egu21-2385
Autor:
František Hrouda, Jan Franěk, Stuart Gilder, Martin Chadima, Josef Ježek, Štěpánka Mrázová, Michal Poňavič, Martin Racek
Publikováno v:
Journal of Structural Geology. 154:104491
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c977eb4c2c7f97869e8b95f6d7858134
https://doi.org/10.1016/j.jsg.2021.104491
https://doi.org/10.1016/j.jsg.2021.104491
Publikováno v:
Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2017, 466, pp.91-102. ⟨10.1016/j.epsl.2017.03.010⟩
Earth and Planetary Science Letters, Elsevier, 2017, 466, pp.91-102. ⟨10.1016/j.epsl.2017.03.010⟩
Most of granulite terrains worldwide are characterized by large mean grain sizes of 1 mm or more. An important exception are the high-pressure felsic granulites in the Bohemian Massif, the European Variscan belt. There, recrystallization of original
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b48b55ed57c23171b84aac89e4836bc
https://hal.archives-ouvertes.fr/hal-01615611
https://hal.archives-ouvertes.fr/hal-01615611
Publikováno v:
Journal of Metamorphic Geology
Journal of Metamorphic Geology, Wiley-Blackwell, 2014, 32 (6), pp.599-626. ⟨10.1111/jmg.12081⟩
Journal of Metamorphic Geology, Wiley-Blackwell, 2014, 32, pp.599-626
Journal of Metamorphic Geology, 2014, 32 (6), pp.599-626. ⟨10.1111/jmg.12081⟩
Journal of Metamorphic Geology, Wiley-Blackwell, 2014, 32 (6), pp.599-626. ⟨10.1111/jmg.12081⟩
Journal of Metamorphic Geology, Wiley-Blackwell, 2014, 32, pp.599-626
Journal of Metamorphic Geology, 2014, 32 (6), pp.599-626. ⟨10.1111/jmg.12081⟩
International audience; We combine structural observations, petrological data and 40Ar-39Ar ages for a stack of amphibolite-facies metasedimentary units that rims high-pressure (HP) granulite-facies felsic bodies exposed in the southern Bohemian Mass
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b51b82f2c201991c64458986ef0709c1
https://hal.archives-ouvertes.fr/hal-01020912
https://hal.archives-ouvertes.fr/hal-01020912
Autor:
Jaroslav Nosek, Milan Brož, Radim Hladký, Vladimír Lachman, Matěj Černý, Jan Uhlík, Jan Franěk
Publikováno v:
Springer Proceedings in Physics ISBN: 9783319055206
This paper describes an evaluation of a newly developed thermally conductive geopolymer (TCG), consisting of a mixture of sodium silicate and carbon micro-particles. The TCG is intended to be used as a component of high temperature energy storage (HT
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::04003c7a38032d36055df769059b6d55
https://doi.org/10.1007/978-3-319-05521-3_32
https://doi.org/10.1007/978-3-319-05521-3_32
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