Abstract
Anisotropy of magnetic susceptibility data for a ferromagnetic granite (Godhra Granite, NW India) are presented and it is shown that the degree of magnetic anisotropy ( P ′) is not controlled by the mean susceptibility ( K m ). Analyses carried out across a high-strain zone lying between granite and adjacent gneiss show that P ′ values are highest in samples that lie close to the contact and decrease away from it. Based on these results it is concluded that if P ′ is not controlled by K m , then the former can be used to gauge strain-intensity variations in ferromagnetic granites.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
