caa a22 4500 465724000 CHVBK 20180323111724.0 cr unu---uuuuu 170327e19901001xx s 000 0 eng 10.1007/BF02316953 doi (NATIONALLICENCE)springer-10.1007/BF02316953 On the detection of weak strain parallel to the bedding by magnetic anisotropy: A mathematical model study [Elektronische Daten] [František Hrouda, Lenka Hrušková] Summary: Five mathematical models of the superposition of deformational magnetic fabric on sedimentary magnetic fabric are presented. These models are represented by various combinations of pure shear and simple shear. The diagrams of the variations in the main magnetic anisotropy parameters with strain can help in recognizing weak ductile deformation in sedimentary rocks. Academia, Publishing House of the Czechoslovak Academy of Sciences, 1990 Hrouda František Geofyzika, N. C., Company Research Institute, Brno aut Hrušková Lenka Geofyzika, N. C., Company Research Institute, Brno aut Studia Geophysica et Geodaetica Kluwer Academic Publishers 34/4(1990-10-01), 327-341 0039-3169 34:4<327 1990 34 11200 https://doi.org/10.1007/BF02316953 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF02316953 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Hrouda František Geofyzika, N. C., Company Research Institute, Brno aut NATIONALLICENCE 700 1- Hrušková Lenka Geofyzika, N. C., Company Research Institute, Brno aut NATIONALLICENCE 773 0- Studia Geophysica et Geodaetica Kluwer Academic Publishers 34/4(1990-10-01), 327-341 0039-3169 34:4<327 1990 34 11200 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer