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Therefore, both the in-plane and axial components of magnetization can be calibrated with a single standard specimen.
After each temperature application, the magnitude of three orthogonal components of magnetization can be measured at room temperature.
The characteristic components of magnetization isolated were used to estimate the vertical-axis rotations occurring during model deformation.
Muxworthy (2010) attempted the Wilson method (Wilson 1962) using the Orion VSM, which is capable of measuring three components of magnetization at elevated temperatures.
In an ordinary spinner magnetometer with a fluxgate sensor, a specimen is rotated about a single axis, and the orientation needs to be manually changed for measuring the three components of magnetization.
Translation of the specimen along the axis allows both the axial and in-plane components of magnetization to produce signals for the radial fluxgate sensor, by decomposition of the signal as described by Kono et al.
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Experimental methods of Alternating Field (AF) demagnetization, Thermal (TH) demagnetization and Isothermal Remanent Magnetization (IRM) experiments are performed to unravel components of magnetizations.
This OOP anisotropy produces an OOP component of magnetization, which is manifested via the formation of magnetic stripe domains, and turned on and off via the applied voltage.
On rotating the sample 90°, the same field of view reveals that the locally inhomogeneous IP component of magnetization is split into a few large domains that coexist with the alternating OOP component of magnetization, which remains visible.
Therefore the IP component of magnetization along the local stripe direction 26– 29 has typically no significant projection onto beam direction.
The IP component of magnetization lies perpendicular to this IP direction, along the same direction in adjacent stripes.
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