作者: P. Rochette , G. Fillion
DOI: 10.1016/0031-9201(88)90079-9
关键词: Anisotropy 、 Geology 、 Pyrrhotite 、 Magnetization 、 Field (physics) 、 Condensed matter physics 、 Instrumentation 、 Magnetite 、 Magnetic susceptibility 、 Magnetometer 、 Mineralogy
摘要: Abstract A new technique involving magnetization measurements on a rotating sample in cryogenic magnetometer with variable field, from 0 to 4 T, and temperature is presented. It can be used separate identify multi-component anisotropy rocks. The results obtained for due magnetite, haematite, pyrrhotite or phyllosilicates are interpreted according different models.