Journal Article10.1016/0040-1951(88)90279-X
Magnetic susceptibility, petrofabrics and strain
493
TL;DR: Magnetic susceptibility is a non-destructive technique for quantifying the average fabric of a small sample of rock as mentioned in this paper, which is not routine substitute for strain analysis, however, the interpretation of the magnetic fabric is not always straightforward and the principal directions of the magnitude ellipsoid of susceptibility commonly show orientations consistent with the kinematic interpretations of folds, shear zones and other structural features.
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About: This article is published in Tectonophysics. The article was published on 10 Dec 1988. The article focuses on the topics: Pure shear & Simple shear.
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Citations
Rock magnetism and the interpretation of anisotropy of magnetic susceptibility
TL;DR: The conventional rules for the interpretation of magnetic susceptibility (AMS) in terms of microstructure and deformation are subject to numerous exceptions as a result of particular rock magnetic effects.
Tectonic applications of magnetic susceptibility and its anisotropy
TL;DR: In this article, the shape of the AMS ellipsoid combines contributions from several different types of AMS components, and the shape changes with the proportions of the different components.
816
Tectonic and sedimentary evolution of the Korean peninsula: a review and new view
TL;DR: A review on the tectonics and sedimentation of major sedimentary basins and orogenic belts (Late Proterozoic-Neogene) in the Korean peninsula is presented in this paper.
767
•Book
Quantitative Textural Measurements in Igneous and Metamorphic Petrology
Michael D. Higgins
- 21 Aug 2006
TL;DR: In this paper, the authors present a review of three dimensional analytical methods for quantitative textural analysis, including general analytical methods, surface and section analytical methods and a detailed analysis of theoretical parameter distributions.
Anisotropy of magnetic susceptibility (AMS): magnetic petrofabrics of deformed rocks
TL;DR: In this paper, the main factors determining the magnetic fabrics of tectonized rocks include mineral-physics properties, crystal symmetry, mineral abundance, mineral-abundances, tectonic symmetry and crystal orientation-distribution, strain or stress, kinematic history and certain tectono-metamorphic processes (e.g., diffusion, crystal plasticity, dynamic recrystallization, particulate flow, neomineralization).
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References
The dependence of weak field susceptibility on applied magnetic field
Guy M. Smith,Subir K. Banerjee +1 more
TL;DR: In this article, it was shown that the apparent potentials that control wall motion are not harmonic but superhamonic for small displacements, which contradicts recent domain wall resonance measurements.
6
The anisotropy of magnetic susceptibility of some igneous and metamorphic rocks
TL;DR: The magnetic ellipsoids of a number of Tertiary lava flows, banded gabbros, dikes, cone sheets, a ring dike, and Precambrian basic gneiss have been determined as discussed by the authors.
Magnetic susceptibility anisotropy of mylonites from the Lake Char mylonite zone, southeastern New England
TL;DR: Magnetic anisotropy data for 72 samples of mylonite and its parent gneiss from the Lake Char mylonitic zone in southeastern New England were presented in this paper.
Magnetic susceptibility anisotropy in the Cambrian slate belt of North Wales and correlation with strain
TL;DR: In this paper, the magnetic susceptibility ellipsoid is oblate for all sites, and the maximum/intermediate susceptibility plane always coincides with the cleavage plane of the slates which has a Caledonian strike and is nearly vertical.
Magnetic susceptibility anisotropy as a strain indicator in the sudbury basin, Ontario
TL;DR: The magnetic susceptibility anisotropy of 181 samples from the Chelmsford Formation, the Onaping Formation and the norite of the Sudbury Basin has been measured as discussed by the authors.