![Figure F4. Concentration-independent parameters as a function of stratigraphic depth for the uppermost 54 m at Site 1165. Normalized anhysteretic susceptibility by low-field susceptibility (kARM/k). Anhysteretic remanent magnetization/isothermal ... Figure F4. Concentration-independent parameters as a function of stratigraphic depth for the uppermost 54 m at Site 1165. Normalized anhysteretic susceptibility by low-field susceptibility (kARM/k). Anhysteretic remanent magnetization/isothermal ...](http://www-odp.tamu.edu/publications/188_SR/015/images/15_f04.gif)
Figure F4. Concentration-independent parameters as a function of stratigraphic depth for the uppermost 54 m at Site 1165. Normalized anhysteretic susceptibility by low-field susceptibility (kARM/k). Anhysteretic remanent magnetization/isothermal ...
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Minerals | Free Full-Text | Particle Size-Specific Magnetic Measurements as a Tool for Enhancing Our Understanding of the Bulk Magnetic Properties of Sediments
![Figure F3. Downcore variations of magnetic parameters (NRM intensity and inclination, magnetic susceptibility, and ARM intensity), relative magnetic grain-size proxy (ARM/k), and magnetic hardness (ARM30 mT/ARM0 mT) determined in Hole 1202A. NRM = Figure F3. Downcore variations of magnetic parameters (NRM intensity and inclination, magnetic susceptibility, and ARM intensity), relative magnetic grain-size proxy (ARM/k), and magnetic hardness (ARM30 mT/ARM0 mT) determined in Hole 1202A. NRM =](http://www-odp.tamu.edu/publications/195_sr/111/images/11_f03.gif)
Figure F3. Downcore variations of magnetic parameters (NRM intensity and inclination, magnetic susceptibility, and ARM intensity), relative magnetic grain-size proxy (ARM/k), and magnetic hardness (ARM30 mT/ARM0 mT) determined in Hole 1202A. NRM =
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Physical Justification for Negative Remanent Magnetization in Homogeneous Nanoparticles | Scientific Reports
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