Figure F67. A. Magnetic domain state of the gabbro rocks. Some samples are identified as multidomain (MD); however, identification of domain state for other samples taken from weak magnetic intensity zones are unsuccessful because of similar anhysteretic remanent magnetization (ARM) and the saturation remanent magnetization (SIRM) curves. B. Magnetic domain state of the sediments above 400 mbsf. Resistance of the ARM relative to the SIRM suggests that single domain states may be dominant in the sediments.

Figure F67. A. Magnetic domain state of the gabbro rocks. Some samples are identified as multidomain (MD); however, identification of domain state for other samples taken from weak magnetic intensity zones are unsuccessful because of similar anhysteretic remanent magnetization (ARM) and the saturation remanent magnetization (SIRM) curves. B. Magnetic domain state of the sediments above 400 mbsf. Resistance of the ARM relative to the SIRM suggests that single domain states may be dominant in the sediments.