Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Martin Chadima"'
Publikováno v:
Geosciences, Vol 12, Iss 6, p 234 (2022)
In anisotropic materials such as minerals and rocks, the AC magnetic susceptibility is also anisotropic, and consists of two components, one in-phase with the applied field (ipMS) and the other out-of-phase (opMS). Correspondingly, anisotropies of th
Externí odkaz:
https://doaj.org/article/77c20a670ed748ffb3d84971112a772c
Autor:
Victor A. Zakharov, Mikhail A. Rogov, Oksana S. Dzyuba, Karel Žák, Martin Košt’ák, Petr Pruner, Petr Skupien, Martin Chadima, Martin Mazuch, Boris L. Nikitenko
Publikováno v:
Polar Research, Vol 33, Iss 0, Pp 1-19 (2014)
The Jurassic/Cretaceous transition was accompanied by significant changes in palaeoceanography and palaeoenvironments in the Tethyan Realm, but outside the Tethys such data are very scarce. Here we present results of a study of the most complete sect
Externí odkaz:
https://doaj.org/article/97bb5ba64e3c4536a931357ee98b1812
Publikováno v:
Studia Geophysica et Geodaetica. 66:187-205
Magnetic susceptibility (both in-phase, ipMS, and out-of-phase, opMS, components) and its anisotropy were investigated in artificial specimens with pure synthetic magnetite and in rocks with titanomagnetite with variable Ti-content reaching XUsp = 0.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c1080303c950c8f57b6d18f121c59a7
https://doi.org/10.5194/egusphere-egu23-2234
https://doi.org/10.5194/egusphere-egu23-2234
Autor:
Jerzy Nawrocki, Olga Rosowiecka, Krystian Wójcik, Martin Chadima, Tomasz Werner, Bogusz Wasik, Marcin Wiewióra
24 brick samples for archaeomagnetic studies were taken from teen historical buildings constructed between c.1280 AD and 1630 AD in northern Poland. Eight of them are from the gothic period. The Thellier-Thellier archaeointensity protocol was used in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4469d6f2c83b5a364b4677c8671cea7
https://doi.org/10.21203/rs.3.rs-2781664/v1
https://doi.org/10.21203/rs.3.rs-2781664/v1
Publikováno v:
Geophysical Journal International. 224:1905-1917
SUMMARY As shown in the literature several times, the calculation of the anisotropy of magnetic susceptibility (AMS) of hematite single crystals using standard linear AMS theory reveals that the calculated minimum principal susceptibility is parallel
In this contribution, we present a rock magnetic and magnetic fabric study of the Dejvice loess/paleosol sequence with an aim to demonstrate how rock magnetic methods can be very effective tools for detecting paleoenvironmental, pedogenic, and post-d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b8abc7d15896778979a0e5f5f5cef511
https://doi.org/10.5194/egusphere-egu22-7202
https://doi.org/10.5194/egusphere-egu22-7202
Out-of-phase component of AC magnetic susceptibility (opMS) in four single crystals of hematite from Minas Gerais, Brazil was investigated. The phase angle ranges from 1° to 6° along the c-axis and slightly exceeds 25° along the basal plane (in th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::616c21988e2523b775042015d5c075ef
https://doi.org/10.5194/egusphere-egu22-4546
https://doi.org/10.5194/egusphere-egu22-4546
Autor:
František Hrouda, Martin Chadima
Publikováno v:
International Journal of Earth Sciences. 109:1321-1336
The magnetic fabrics in sedimentary, volcanic, and plutonic rocks primarily originate during deposition, lava or ash flow, and magma flow, respectively. During later rock development, these magnetic fabrics can be overprinted by various processes amo
Autor:
Josef Jezek, Martin Chadima
The growing interest in ferromagnetic fabric, i.e. magnetic fabric carried solely by ferromagnetic (sensu lato) grains, creates the need for a simple way to obtain anisotropy of magnetic remanence (AMR) tensors from a set of laboratory imparted, spat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::969e0586ce206a63ea9073887a6b4c6b
https://doi.org/10.5194/egusphere-egu21-1155
https://doi.org/10.5194/egusphere-egu21-1155