Numerical estimation of a tsunami source at the flexural area of Kuril and Japan Trenches in the fifteenth to seventeenth century based on paleotsunami deposit distributions in northern Japan

Progress in Earth and Planetary Science

Table 4 Fault parameters of newly proposed models with 6, 10, 14, and 18 m slip amounts

Fault model		Depth (km)	Length (km)	Width (km)	Dip (°)	Strike (°)	Rake (°)	Slip (m)	Mw*
S	S1	5	150	100	11	215	90	6	8.30
	S1	5	150	100	11	215	90	10	8.45
	S1	5	150	100	11	215	90	14	8.55
	S1	5	150	100	11	215	90	18	8.62
	S2	24	150	100	21	215	90	6	8.30
	S2	24	150	100	21	215	90	10	8.45
	S2	24	150	100	21	215	90	14	8.55
	S2	24	150	100	21	215	90	18	8.62
T	T1	5	150	100	10	205	90	6	8.30
	T1	5	150	100	10	205	90	10	8.45
	T1	5	150	100	10	205	90	14	8.55
	T1	5	150	100	10	205	90	18	8.62
	T2	22	150	100	20	205	90	6	8.30
	T2	22	150	100	20	205	90	10	8.45
	T2	22	150	100	20	205	90	14	8.55
	T2	22	150	100	20	205	90	18	8.62
U	U1	5	150	100	9	195	90	6	8.30
	U1	5	150	100	9	195	90	10	8.45
	U1	5	150	100	9	195	90	14	8.55
	U1	5	150	100	9	195	90	18	8.62
	U2	21	150	100	17	195	90	6	8.30
	U2	21	150	100	17	195	90	10	8.45
	U2	21	150	100	17	195	90	14	8.55
	U2	21	150	100	17	195	90	18	8.62