Geophysical surveys

, Volume 5, Issue 1, pp 37–82

Magnetic anisotropy of rocks and its application in geology and geophysics

  • František Hrouda

DOI: 10.1007/BF01450244

Cite this article as:
Hrouda, F. Geophysical Surveys (1982) 5: 37. doi:10.1007/BF01450244


Magnetic anisotropy in sedimentary rocks is controlled by the processes of deposition and compaction, in volcanic rocks by the lava flow and in metamorphic and plutonic rocks by ductile deformation and mimetic crystallization. In massive ore it is due to processes associated with emplacement and consolidation of an ore body as well as to ductile deformation. Hence, it can be used as a tool of structural analysis for almost all rock types. Morcover, it can influence considerably the orientation of the remanent magnetization vector as well as the configuration of a magnetic anomaly over a magnetized body. For these reasons it should be investigated in palaeomagnetism and applied geophysics as well.

Copyright information

© D. Reidel Publishing Company 1982

Authors and Affiliations

  • František Hrouda
    • 1
  1. 1.Geofyzika, národní podnikBrnoCzechoslovakia