Abstract
Minnesotaite, a 2:1 layer sheet silicate, is antifer-romagnetic below 30 K. A spin flop or metamagnetic transition occurs in a small applied magnetic field. Neutron diffraction and Mossbauer spectroscopy, in an external magnetic field of 4.0 T, show that the magnetic structure consists of Fe2+ spins coupled ferromagnetically in the c plane with alternate ferromagnetic planes coupled antiferromagnetically.
Sign-in/Register to access full text options 
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.
