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Magnetic Anisotropy of Rocks: A New Classification of Inverse Magnetic Fabrics to Help Geological Interpretations

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F20%3A00535495" target="_blank" >RIV/67985831:_____/20:00535495 - isvavai.cz</a>

  • Alternative codes found

    RIV/68378271:_____/20:00535495 RIV/00216224:14310/20:00117028

  • Result on the web

    <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JB020426" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020JB020426</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1029/2020JB020426" target="_blank" >10.1029/2020JB020426</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Magnetic Anisotropy of Rocks: A New Classification of Inverse Magnetic Fabrics to Help Geological Interpretations

  • Original language description

    Inverse magnetic fabrics defined by anisotropy of magnetic susceptibility with the longest principal axis perpendicular to bedding were identified in the studied samples of Ordovician sedimentary rocks from the Barrandian area, Czech Republic. These fabrics are related to ankerite fibers in association with cone-in-cone structures. To understand the meaning of such inverse magnetic fabrics for geological interpretations, a new, more detailed classification of inverse magnetic fabrics' types is formulated in this paper. Distinguishing the structural (i.e., shape) and magnetocrystalline anisotropies in rocks, three new (sub)types of magnetic fabrics were defined in this study based on the combination of structural normal/inverse and magnetocrystalline normal/inverse anisotropies. As a result, normal magnetic fabric is extended by new fabric types associated with inverse anisotropy: simple inverse, pure inverse, and pseudo-normal magnetic fabrics. The studied fibrous ankerite shows simple inverse magnetic fabric, which results from the combination of normal magnetocrystalline and inverse structural anisotropies.

  • 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

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2020

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Journal of Geophysical Research: Solid Earth

  • ISSN

    2169-9313

  • e-ISSN

  • Volume of the periodical

    125

  • Issue of the periodical within the volume

    11

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    13

  • Pages from-to

    e2020JB020426

  • UT code for WoS article

    000595735100003

  • EID of the result in the Scopus database

    2-s2.0-85096464156