Earth, Planets and Space

Table 2 Slip-deficit rates and subsidence rates (MSL_{3 kyr BP} = 0 m)

From: The source model and recurrence interval of Genroku-type Kanto earthquakes estimated from paleo-shoreline data

Case	Slip-deficit rate				Subsidence rate
	Miura		Southernmost Boso		Aburatsubo	Mera
	Site no. 1		Site no. 16		Site no. 3	Site no. 19
	S_G	R_d	S_G	R_d	R_S	R_S
	m	cm/year	m	cm/year	mm/year	mm/year
300_2	18 ± 15	4.3 ± 2.5	30 ± 11	6.0 ± 1.8	−3.41 ± 1.07	−11.31 ± 1.07
300_3	16 ± 11	3.6 ± 1.2	24 ± 9	4.0 ± 1.0	−3.44 ± 0.85	−6.62 ± 0.85
300_4	14 ± 9.5	3.2 ± 0.8	21 ± 7.5	3.3 ± 0.7	−3.46 ± 0.83	−5.01 ± 0.83
300_5	13 ± 9.5	3.0 ± 0.7	20 ± 7.5	2.9 ± 0.6	−3.46 ± 0.79	−4.23 ± 0.79
300_6	14 ± 9	3.0 ± 0.6	20 ± 7	2.8 ± 0.5	−3.46 ± 0.78	−3.75 ± 0.78
300_7	14 ± 9	3.0 ± 0.5	20 ± 7	2.7 ± 0.4	−3.46 ± 0.77	−3.43 ± 0.77
350_2	13 ± 12	3.0 ± 1.7	25 ± 10	4.4 ± 1.4	−2.24 ± 0.98	−6.57 ± 0.98
350_3	12 ± 10	2.7 ± 1.0	21 ± 7.5	3.1 ± 0.7	−2.50 ± 0.86	−3.74 ± 0.86
350_4	12 ± 9.5	2.6 ± 0.7	19 ± 7.5	2.6 ± 0.6	−2.58 ± 0.80	−2.73 ± 0.80
350_5	13 ± 9	2.6 ± 0.6	19 ± 7	2.5 ± 0.5	−2.63 ± 0.78	−2.18 ± 0.78
350_6	12 ± 9	2.5 ± 0.5	19 ± 7	2.3 ± 0.4	−2.66 ± 0.77	−1.85 ± 0.77
400_2	12 ± 12	2.5 ± 1.5	23 ± 9	3.6 ± 1.1	−1.53 ± 0.89	−3.80 ± 0.89
400_3	11 ± 9.5	2.3 ± 0.8	20 ± 7.5	2.7 ± 0.6	−1.86 ± 0.83	−1.86 ± 0.83
400_4	12 ± 9	2.3 ± 0.6	19 ± 7	2.3 ± 0.5	−1.98 ± 0.79	−1.13 ± 0.79
400_5	11 ± 9	2.2 ± 0.5	18 ± 7	2.1 ± 0.4	−2.05 ± 0.77	−0.74 ± 0.77
400_6	11 ± 9	2.1 ± 0.4	18 ± 7	2.0 ± 0.4	−2.09 ± 0.76	−0.50 ± 0.76

Italicized data indicate that the relative plate velocity (2.7 cm/year) is included within the range of calculated slip-deficit rate ± one standard deviation and that the observed subsidence rate (−3.05 mm/year at Aburatsubo, −2.57 mm/year at Mera) is included within the range of calculated subsidence rate ± one standard deviation
S _G slip amount, R _d slip-deficit rate, R _S subsidence rate

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