Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Leonid Surovitskii"'
Autor:
Dmitriy O. Testov, Kamil G. Gareev, Ivan K. Khmelnitskiy, Andrei Kosterov, Leonid Surovitskii, Victor V. Luchinin
Publikováno v:
Magnetochemistry, Vol 9, Iss 1, p 10 (2022)
ε-Fe2O3 is an iron(III) oxide polymorph attracting an increasing interest due to its unique magnetic properties combining extremely high coercivity and relatively large saturation magnetization. We review existing methods for the ε-Fe2O3 synthesis
Externí odkaz:
https://doaj.org/article/7cf4abfe0d9a4a0bac3779bf44643177
Publikováno v:
Springer Proceedings in Earth and Environmental Sciences ISBN: 9783030914660
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a560212bb0ce4bcbe2c992e2d45fc96
https://doi.org/10.1007/978-3-030-91467-7_8
https://doi.org/10.1007/978-3-030-91467-7_8
Publikováno v:
Journal of Archaeological Science. 144:105639
Autor:
Mary Kovacheva, Andrei Kosterov, Aleksey V. Smirnov, Maria Kostadinova-Avramova, Natalya Salnaya, Leonid Surovitskii
The three-axis isothermal remanent magnetization (IRM) test (the Lowrie test; Lowrie, 1990, Geophys. Res. Lett., 17, 159-162) is a useful tool to identify ferromagnetic minerals by their coercivity and unblocking temperature spectra. In this study, w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::280f7c223e7ce07fa50e8fb33e395055
https://doi.org/10.5194/egusphere-egu21-1782
https://doi.org/10.5194/egusphere-egu21-1782
Ti-rich titanomagnetite is a primary magnetic mineral in submarine basalts, as well as in some terrestrial volcanic rocks. On geological timescale, it undergoes a slow oxidation forming titanomaghemites. This natural process may be modeled to some ex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b968ace7bc0cb203555c56f951e46833
https://doi.org/10.5194/egusphere-egu21-1980
https://doi.org/10.5194/egusphere-egu21-1980
Autor:
P. Minaev, Andrei Kosterov, Svetlana Yu. Yanson, Leonid Surovitskii, Maria Kostadinova-Avramova, P. V. Kharitonskii, E. S. Sergienko, Mary Kovacheva, Natalia Salnaia
SUMMARYThe thorough understanding of magnetic mineralogy is a prerequisite of any successful palaeomagnetic or archaeomagnetic study. Magnetic minerals in archaeological ceramics and baked clay may be inherited from the parent material or, more frequ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e83196a9ca8ce21fc889e0d130febe61
Publikováno v:
Journal of Geophysical Research: Solid Earth.
Nonheating paleointensity methods utilize an anhysteretic remanent magnetization (ARM) or a saturation isothermal remanent magnetization to model the natural thermal remanent magnetization (TRM) to avoid heating-induced alteration. We report the resu