Shaoying He, Shiwei Sun, Tongchun Xu
Abstract
Astatic magnetometers, operating within the Earth's magnetic field, can be used to measure simultaneously the magnetic remanence and anisotropy of magnetic susceptibility ellipsoid of cubic or cylindrical rock and ore samples with susceptibilities greater than 3 × 10−4 SI.
OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Astatic magnetometers, operating within the Earth's magnetic field, can be used to measure simultaneously the magnetic remanence and anisotropy of magnetic susceptibility ellipsoid of cubic or cylindrical rock and ore samples with susceptibilities greater than 3 × 10−4 SI.
Key concepts: Magnetometer, Remanence, Ellipsoid, Anisotropy, Magnetic field, Geology, Measure (data warehouse), Geophysics