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Progress in Earth and Planetary Science
Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

From: Submarine paleoseismology in the Japan Trench of northeastern Japan: turbidite stratigraphy and sedimentology using paleomagnetic and rock magnetic analyses

Fig. 6

Declination and inclination data after removal of turbidite intervals: a declination of KS1416PC06, b declination of KS1416PC07, c declination of Archeo3k.1. d inclination of KS1416PC06, e inclination of KS1416PC07, f inclination n of Archeo3k.1, respectively. ΔD95 and ΔI95 are also shown for declinations and inclinations. Broken lines indicate the horizon of turbidite beds. A–D, a–e are tie points used in correlation between core data and Arche3k.1. g Fitting KS1416PC06 declination data (red line) to that of Arche3k.1(gray line), h KS1416PC06 inclination data (red line) to that of Arche3k.1(gray line), i KS1416PC07 declination data (red line) to that of Arche3k.1(gray line), j KS1416PC07 inclination data (red line) to that of Arche3k.1(gray line)

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