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.
Реэюме
Пруво¶rt;umся nяmь мamемamuческuх мо¶rt;елеŭ суnерnозuцuu ¶rt;еформaцuонноŭ мa¶rt;нumноŭ mексmуры на осa¶rt;очноŭ мa¶rt;нumноŭ mексmуре. Мо¶rt;елu ире¶rt;сmвaлены в рaзных комбuнaцuях чuсmо¶rt;о с¶rt;вu¶rt;а ц иросmо¶rt;о с¶rt;вu¶rt;а. Дua¶rt;раaммы вaрuaцuŭ в ¶rt;лaвных naрaмеmрaх мa¶rt;нumноŭ aнuзоmроnuu с ¶rt;еформaцuеŭ мо¶rt;уm nомочь nрu рaсnознaвaнuu слaбых nлaсmuчных ¶rt;еформaцŭŭ в осa¶rt;очных nоро¶rt;aх.
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Hrouda, F., Hrušková, L. On the detection of weak strain parallel to the bedding by magnetic anisotropy: A mathematical model study. Stud Geophys Geod 34, 327–341 (1990). https://doi.org/10.1007/BF02316953
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DOI: https://doi.org/10.1007/BF02316953