Frequency-dependent AMS of rocks: A tool for the investigation of the fabric of ultrafine magnetic particles
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10287223" target="_blank" >RIV/00216208:11310/14:10287223 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.tecto.2014.01.040" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2014.01.040</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.tecto.2014.01.040" target="_blank" >10.1016/j.tecto.2014.01.040</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Frequency-dependent AMS of rocks: A tool for the investigation of the fabric of ultrafine magnetic particles
Popis výsledku v původním jazyce
In some geological processes, new very fine-grained magnetic minerals may originate. The variation in content of these minerals is routinely investigated by frequency-dependent magnetic susceptibility, which is traditionally interpreted in terms of the presence of viscous superparamagnetic (SP) particles in addition to stable single domain (SSD) and multidomain (MD) magnetic particles. In addition, the fabric of these grains can be investigated through the frequency-dependent AMS. Through standard AMS measurement at different frequencies, one can evaluate the contribution of SP particles to the whole-rock AMS; appropriate methods were developed. Various rocks, soils and ceramics, showing frequency-dependent magnetic susceptibility, were investigated. Measurable changes of AMS with operating frequency were revealed and attempts are made of their fabric interpretation. (C) 2014 Elsevier B.V. All rights reserved.
Název v anglickém jazyce
Frequency-dependent AMS of rocks: A tool for the investigation of the fabric of ultrafine magnetic particles
Popis výsledku anglicky
In some geological processes, new very fine-grained magnetic minerals may originate. The variation in content of these minerals is routinely investigated by frequency-dependent magnetic susceptibility, which is traditionally interpreted in terms of the presence of viscous superparamagnetic (SP) particles in addition to stable single domain (SSD) and multidomain (MD) magnetic particles. In addition, the fabric of these grains can be investigated through the frequency-dependent AMS. Through standard AMS measurement at different frequencies, one can evaluate the contribution of SP particles to the whole-rock AMS; appropriate methods were developed. Various rocks, soils and ceramics, showing frequency-dependent magnetic susceptibility, were investigated. Measurable changes of AMS with operating frequency were revealed and attempts are made of their fabric interpretation. (C) 2014 Elsevier B.V. All rights reserved.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/GA13-06958S" target="_blank" >GA13-06958S: Záznam minerálních a texturních znaků před exhumačního a před kolizního vývoje HP/UHP hornin v orogenní zóně</a><br>
Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Tectonophysics
ISSN
0040-1951
e-ISSN
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Svazek periodika
629
Číslo periodika v rámci svazku
August
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
12
Strana od-do
27-38
Kód UT WoS článku
000341474600004
EID výsledku v databázi Scopus
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