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Examples of tectonic overprints of magnetic fabrics in rocks of the Bohemian Massif and Western Carpathians

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F20%3A00524710" target="_blank" >RIV/67985831:_____/20:00524710 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/20:10420434

  • Result on the web

    <a href="https://link.springer.com/article/10.1007/s00531-019-01786-8" target="_blank" >https://link.springer.com/article/10.1007/s00531-019-01786-8</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00531-019-01786-8" target="_blank" >10.1007/s00531-019-01786-8</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Examples of tectonic overprints of magnetic fabrics in rocks of the Bohemian Massif and Western Carpathians

  • Original language description

    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 among which regional metamorphism and ductile deformation tectonic in origin are probably the most frequent and important. During the overprinting, the degree of anisotropy in general increases with progressing deformation and the magnetic foliations and magnetic lineations are reoriented from the primary directions towards parallelism to the doubtless deformational fabric elements in the body considered or in surrounding rocks. Because of the second rank tensor character of the anisotropy of magnetic susceptibility (AMS) it is often difficult to recognize whether a particular magnetic fabric was overprinted or not. The identification techniques of the magnetic fabric overprints on the site scale were developed, which are based on the investigation of the relationship between the magnetic fabric and orientations of mesoscopic fabric elements whose origin is known (bedding, cleavage, metamorphic foliation, mineral lineation, fold axis, etc.) and on the investigation of fabric relationship between geological units of different origins, because the AMS can be measured with sufficient precision in virtually all rock types.

  • 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/GA18-03160S" target="_blank" >GA18-03160S: Pre- to syncollisional history of metamorphic rocks in orogenic zone recorded by chemical zoning in garnet; with application to the Bohemian Massif</a><br>

  • 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

    International Journal of Earth Sciences

  • ISSN

    1437-3254

  • e-ISSN

  • Volume of the periodical

    109

  • Issue of the periodical within the volume

    4

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    16

  • Pages from-to

    1321-1336

  • UT code for WoS article

    000538414100010

  • EID of the result in the Scopus database

    2-s2.0-85075352442