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Fig. 5 | Progress in Earth and Planetary Science

Fig. 5

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

Fig. 5

a, e declination data with 0° (gray broken line) for cores KS1416PC06 and KS1416PC07, and b, d inclination data with GAD inclination (gray broken line) for cores KS1416PC06 and KS1416PC07, respectively. ΔD95 and ΔI95 (Khokhlov and Hulot 2016) shown with declinations and inclinations. Gray hatched intervals indicate turbidite beds

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