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Fundamental relations of mineral specific magnetic carriers for paleointensity determination

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F17%3A10363669" target="_blank" >RIV/00216208:11310/17:10363669 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985831:_____/17:00481730

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.pepi.2017.09.008" target="_blank" >http://dx.doi.org/10.1016/j.pepi.2017.09.008</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.pepi.2017.09.008" target="_blank" >10.1016/j.pepi.2017.09.008</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Fundamental relations of mineral specific magnetic carriers for paleointensity determination

  • Original language description

    A fundamental linear relationship exists between the efficiency of thermoremanent magnetization measured at room temperature and the magnitude of the ambient field at the time of acquisition. The magnetic efficiency (the ratio of thermoremanent magnetization to saturation remanent magnetization) multiplied by the saturation mag-netization is proportional to the magnetizing field, where the proportionality constant is independent of magnetic mineralogy and domain state. The empirical constant for this equation was determined using existing experimen-tal data of single domain through pseudosingle domain to multidomain states of iron, meteoritic iron, magnetite, maghemite, pyrrhotite, and hematite. We show that the acquired magnetic efficiency is closely related to two types of demagnetizing fields that act as barriers against domain wall pinning during magnetic acquisition. The first relates to the saturation magnetization that is derived from the distribution of Bohr magnetons within the crystal lattice, and the second originates from grain shape. Theoretical considerations imply a factor of two dif-ference in the magnetic efficiency acquired during laboratory and geologic timescales. This equation reveals that troilite may be a potentially important magnetic carrier for extraterrestrial magnetism. Using magnetic scanning techniques, our relationship allows for estimating the paleointensity from samples that contain more than one magnetic species.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

    <a href="/en/project/GA17-05935S" target="_blank" >GA17-05935S: Role of changes in environemntal chemistry on lake ecosystems at the Younger Dryas onset</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2017

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Physics of the Earth and Planetary Interiors

  • ISSN

    0031-9201

  • e-ISSN

  • Volume of the periodical

    neuveden

  • Issue of the periodical within the volume

    septembre

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    7

  • Pages from-to

  • UT code for WoS article

    000415773900005

  • EID of the result in the Scopus database