Skip to main content

Table 1 Characteristics of the earthquakes used in the analysis

From: Velocity increase in the uppermost oceanic crust of subducting Philippine Sea plate beneath the Kanto region due to dehydration inferred from high-frequency trapped P waves

Number

Origin time (local time)

Longitude

Latitude

Depth (km)

Mw

1

4 April 2008 19:01

139.828

36.120

56.0

4.8

2

2 April 2011 16:55

139.962

36.207

56.0

4.8

3

26 April 2011 21:12

139.976

36.086

59.0

4.9

4

11 February 2012 10:26

139.789

36.088

59.0

4.8

5

18 May 2012 17:18

139.841

36.136

59.0

4.8

6

16 July 2012 04:31

139.817

36.152

62.0

4.8

7

1 February 2013 01:04

139.893

36.056

50.0

4.3