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Paleoclimatic and provenance implications of magnetic parameters from the Miocene sediments in the Subei Basin
![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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Bi-plot summary of the median destructive field of the Anhysteretic... | Download Scientific Diagram
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![Figure F3. A. Stepwise demagnetization of natural remanent magnetization (NRM). B. Stepwise acquisition of anhysteretic remanent magnetization (ARM) for 29 discrete samples from Hole 1225C. C. Demagnetization plot of typical sample from Figure F3. A. Stepwise demagnetization of natural remanent magnetization (NRM). B. Stepwise acquisition of anhysteretic remanent magnetization (ARM) for 29 discrete samples from Hole 1225C. C. Demagnetization plot of typical sample from](http://www-odp.tamu.edu/publications/201_SR/110/images/10_f03.gif)