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

Fig. 2

From: Possible climate preconditioning on submarine landslides along a convergent margin, Nankai Trough (NE Pacific)

Fig. 2

Seismic reflection profile showing the stratigraphic succession of the lower slope basin downslope of the forearc high and the megasplay fault zone (MSF). The multiple stacked MTD features (dashed black lines represent the bases of MTDs, continuous black lines the tops of the MTDs) can be identified on the seismic reflection profile. Bottom-simulating reflector (BSR; white dashed line) is indicative of the occurrence of gas hydrate-laden sediments. Site C0018 (black bar) is located within the slope basin. SU1a seismic unit 1a, SU1b seismic unit b (white transparent area marks the limits of SU1b)

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