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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
Literature data on single crystals of graphite shows that this mineral is diamagnetic and strongly anisotropic. In addition, it possesses high electrical conductivity and extremely strong conductivity anisotropy. The AC magnetic susceptibility of gra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba2a824905583db43b83272ea8430dfe
https://doi.org/10.5194/egusphere-egu2020-2868
https://doi.org/10.5194/egusphere-egu2020-2868
Publikováno v:
Geoscience Research Reports. :57-62
Publikováno v:
Geoscience Research Reports.
Publikováno v:
Geoscience Research Reports.