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Fig. 6 | Earth, Planets and Space

Fig. 6

From: Timing of clockwise rotation of Southwest Japan: constraints from new middle Miocene paleomagnetic results

Fig. 6

Representative results of stepwise thermal demagnetization of three-axis IRM produced in steady fields at 3.0 T (hard component), 0.40 T (medium component), and 0.12 T (soft component). Variations in the low-field magnetic susceptibility (MS) with temperature are also shown. Names in square brackets are sample designations used in the laboratory. a E12 [12-1a] tuff. b W23 [J2-2c] siltstone. c W29 [O-2a] siltstone

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