![Figure 9. Plot of the characteristic remanent magnetization (inclination and declination) from u-channel measurements and normalized remanence record of the B-M transition at Site 1014. Natural remanent magnetization (NRM) and anhysteretic remanent Figure 9. Plot of the characteristic remanent magnetization (inclination and declination) from u-channel measurements and normalized remanence record of the B-M transition at Site 1014. Natural remanent magnetization (NRM) and anhysteretic remanent](http://www-odp.tamu.edu/publications/167_SR/chap_28/images/08_f09.jpg)
Figure 9. Plot of the characteristic remanent magnetization (inclination and declination) from u-channel measurements and normalized remanence record of the B-M transition at Site 1014. Natural remanent magnetization (NRM) and anhysteretic remanent
![Proc. IODP, 303/306, Data report: magnetic properties of unconsolidated deep-sea sediments from the North Atlantic, IODP Expedition 303 Sites U1302–U1304 and U13081 Proc. IODP, 303/306, Data report: magnetic properties of unconsolidated deep-sea sediments from the North Atlantic, IODP Expedition 303 Sites U1302–U1304 and U13081](http://publications.iodp.org/proceedings/303_306/209/images/F03.gif)
Proc. IODP, 303/306, Data report: magnetic properties of unconsolidated deep-sea sediments from the North Atlantic, IODP Expedition 303 Sites U1302–U1304 and U13081
![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 =
![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 ...
Astudy of anhysteretic remanent magnetization with the variation of A. C. and D. C. fields on Rajmahal basalts
![Proc. IODP, 303/306, Data report: magnetic properties of unconsolidated deep-sea sediments from the North Atlantic, IODP Expedition 303 Sites U1302–U1304 and U13081 Proc. IODP, 303/306, Data report: magnetic properties of unconsolidated deep-sea sediments from the North Atlantic, IODP Expedition 303 Sites U1302–U1304 and U13081](http://publications.iodp.org/proceedings/303_306/209/images/F04.gif)
Proc. IODP, 303/306, Data report: magnetic properties of unconsolidated deep-sea sediments from the North Atlantic, IODP Expedition 303 Sites U1302–U1304 and U13081
![Minerals | Free Full-Text | Integrated Magnetic Analyses for the Discrimination of Urban and Industrial Dusts Minerals | Free Full-Text | Integrated Magnetic Analyses for the Discrimination of Urban and Industrial Dusts](https://www.mdpi.com/minerals/minerals-10-01056/article_deploy/html/images/minerals-10-01056-g004a.png)
Minerals | Free Full-Text | Integrated Magnetic Analyses for the Discrimination of Urban and Industrial Dusts
![Remanence cycling of 0.6–135 µm magnetites across the Verwey transition | Earth, Planets and Space | Full Text Remanence cycling of 0.6–135 µm magnetites across the Verwey transition | Earth, Planets and Space | Full Text](https://media.springernature.com/lw685/springer-static/image/art%3A10.1186%2Fs40623-018-0928-z/MediaObjects/40623_2018_928_Fig1_HTML.png)