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

J 2020

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

ČERNÝ, Jan; Rostislav MELICHAR; Dalibor VŠIANSKÝ a Jan DRAHOKOUPIL

Základní údaje

Originální název

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

Autoři

ČERNÝ, Jan (203 Česká republika); Rostislav MELICHAR (203 Česká republika, domácí); Dalibor VŠIANSKÝ (203 Česká republika, domácí) a Jan DRAHOKOUPIL (203 Česká republika)

Vydání

Journal of Geophysical Research: Solid Earth, Washington, D.C. American Geophysical Union, 2020, 2169-9313

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10505 Geology

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Odkazy

Odkaz na plný text článku

Impakt faktor

Impact factor: 3.848

Kód RIV

RIV/00216224:14310/20:00117028

Organizační jednotka

Přírodovědecká fakulta

DOI

http://dx.doi.org/10.1029/2020JB020426

UT WoS

000595735100003

EID Scopus

2-s2.0-85096464156

Klíčová slova česky

anizotropie magnetické susceptibility; barrandien; inverzní magnetická stavba; sedimentární horniny

Klíčová slova anglicky

anisotropy of magnetic susceptibility; Barrandian; inverse magnetic anisotropy; sedimentary rocks

Štítky

barrandian, barrandien, Magnetic fabric, magnetic susceptibility, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 4. 1. 2021 19:14, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

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.

Citovat

ČERNÝ, Jan; Rostislav MELICHAR; Dalibor VŠIANSKÝ a Jan DRAHOKOUPIL. Magnetic Anisotropy of Rocks: A New Classification of Inverse Magnetic Fabrics to Help Geological Interpretations. Journal of Geophysical Research: Solid Earth. Washington, D.C.: American Geophysical Union, 2020, roč. 125, č. 11, s. 1-13. ISSN 2169-9313. Dostupné z: https://dx.doi.org/10.1029/2020JB020426.

@article{1697116,
   author = {Černý, Jan and Melichar, Rostislav and Všianský, Dalibor and Drahokoupil, Jan},
   article_location = {Washington, D.C.},
   article_number = {11},
   doi = {http://dx.doi.org/10.1029/2020JB020426},
   keywords = {anisotropy of magnetic susceptibility; Barrandian; inverse magnetic anisotropy; sedimentary rocks},
   language = {eng},
   issn = {2169-9313},
   journal = {Journal of Geophysical Research: Solid Earth},
   title = {Magnetic Anisotropy of Rocks: A New Classification of Inverse Magnetic Fabrics to Help Geological Interpretations},
   url = {https://doi.org/10.1029/2020JB020426},
   volume = {125},
   year = {2020}
}

TY  - JOUR
ID  - 1697116
AU  - Černý, Jan - Melichar, Rostislav - Všianský, Dalibor - Drahokoupil, Jan
PY  - 2020
TI  - Magnetic Anisotropy of Rocks: A New Classification of Inverse Magnetic Fabrics to Help Geological Interpretations
JF  - Journal of Geophysical Research: Solid Earth
VL  - 125
IS  - 11
SP  - 1-13
EP  - 1-13
PB  - American Geophysical Union
SN  - 21699313
KW  - anisotropy of magnetic susceptibility
KW  - Barrandian
KW  - inverse magnetic anisotropy
KW  - sedimentary rocks
UR  - https://doi.org/10.1029/2020JB020426
L2  - https://doi.org/10.1029/2020JB020426
N2  - 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.
ER  -

ČERNÝ, Jan; Rostislav MELICHAR; Dalibor VŠIANSKÝ a Jan DRAHOKOUPIL. Magnetic Anisotropy of Rocks: A New Classification of Inverse Magnetic Fabrics to Help Geological Interpretations. \textit{Journal of Geophysical Research: Solid Earth}. Washington, D.C.: American Geophysical Union, 2020, roč.~125, č.~11, s.~1-13. ISSN~2169-9313. Dostupné z: https://dx.doi.org/10.1029/2020JB020426.

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