Magnetic fabric in folds of the easternmost Rheno-Hercynian Zone

Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy

Volumn 25, Issue 5, 2000, Pages 505-510

  Hrouda, F ^a,b   Krejci O ^c   Otava, J ^c  

^a Advanced Geoscience Instruments Company   (Czech Republic)

^b CHARLES UNIVERSITY   (Czech Republic)

^c CZECH GEOLOGICAL SURVEY   (Czech Republic)

Author keywords

[No Author keywords available]

Indexed keywords

DEFORMATION MECHANISM; FOLD; MAGNETIC ANISOTROPY; MAGNETIC PROPERTY; METAMORPHISM;

CZECH REPUBLIC;

EID: 0033865527     PISSN: 14641895     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1464-1895(00)00078-8     Document Type: Article

References (5)

1. Dvořák, J., and M. Wolf, 1979.Thermal metamorphism in the Moravian Palaeozoic (Sudeticum, Č.S.S.R), Neues Jahrb. Geol. Palaeontol. Monatsh., 1979, 596-607.
2. Hrouda, F., 1978. The magnetic fabric in some folds, Phys. Earth Planet. Inter., 77, 89-97.
3. Hrouda, F., 1979. The strain interpretation of magnetic anisotropy in rocks of the Nízký Jeseník Mountains (Czechoslovakia). Sb. Geol. Věd, UG, 16, 27-62.
4. Hrouda, F., 1981. On the mechanism of the fold generation in the nízký Jeseník Mts. (in Czech). Věst. Ústř. Úst. Geol., 56, 271-278.
5. Hrouda, F., Pros, Z. and Wohlgemuth, J., 1993. Development of magnetic and elastic anisotropies in slates during progressive deformation. Phys. Earth Planet. Inter., 77, 1993, 251-265.