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Progress in Earth and Planetary Science
Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

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

Fig. 2

Lithology and magnetic properties of core a KS1416PC06; b KS1416PC07; c photo, lithology, magnetic properties of turbidite of P6t4 in KS1416PC06; d photo, lithology, magnetic properties of turbidite of P7t1 in KS1416PC07. MS: magnetic susceptibility; ARM/MS: ratio of Anhysteretic remanent magnetization (ARM) and MS; L: magnetic lineation (red line); F: magnetic foliation (blue line). Lithology columns are based on Ikehara et al. (2017). Legend for lithological columns: white, bioturbated diatomaceous clay-silty clay; gray, homogeneous diatomaceous clay-silty clay; blue, homogeneous nannofossil-bearing diatomaceous mud; red, volcanic ash; black thick line, sand bed; dark gray, coarse silt bed. Yellow hatches in MS, ARM/MS, L and F columns reveal the intervals of turbidite beds. The turbidite beds are labeled sequentially as P6t1 to P6t9 and P7t1 to P7t6. “P6” and “P7” stand for the core IDs “KS1416PC06” and “KS1416PC07.” “t” stands for turbidite, and “1” through “9” is the number of the turbidite deposit from the top to the base of the core

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