Fig. 7From: Preliminary paleomagnetic and rock magnetic results from 17 to 22 ka sediment of Jeju Island, Korea: Geomagnetic excursional behavior or rock magnetic anomalies?Results of a high-temperature weak-field thermomagnetic (k–T) curve, b high-temperature strong-field thermomagnetic (Ms–T) curve, and c STHD of 3-axis IRMs with different coercivities (Lowrie 1990), from selected horizons (7, 29, 33 and 39 cm depth of the GSDS1 profile)Back to article page