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Table 2 Inversion results for each case

From: Joint inversion of strain and tilt data using the Akaike’s Bayesian information criterion to map detailed slip distributions of short-term slow slip events

Case

Seismic moment (N m)

Moment magnitude

Standard deviation/slip (cm)a

N170E

N80E

Example 1: 14–19 April 2015

7.99 × 1017

5.87

0.18/1.15

0.19/0.56

 Rectangle fault model

1.25 × 1018

6.00

  

 Based on strain data alone

3.20 × 1017

5.60

0.43/0.56

0.33/0.65

 Rectangle fault model

1.54 × 1018

6.06

  

 Based on tilt data alone

0.36/0.97

0.40/0.26

 Rectangle fault model

1.27 × 1018

6.00

  

Example 2: 29 December 2015 to 1 January 2016

6.05 × 1017

5.79

0.07/0.25

0.07/0.36

 Rectangle fault model

3.81 × 1017

5.65

  

Example 2: 1–5 January 2016

6.67 × 1017

5.82

0.20/0.61

0.16/0.86

 Rectangle fault model

6.14 × 1017

5.79

  

Example 2: 5–7 January 2016

1.56 × 1017

5.40

0.07/0.30

0.07/0.15

 Rectangle fault model

4.28 × 1017

5.69

  

Example 3: 23–27 October 2016

6.92 × 1017

5.83

0.23/0.89

0.25/0.42

 Rectangle fault model

1.16 × 1018

5.98

  

 Based on strain data alone

2.05 × 1017

5.47

0.15/0.17

0.15/0.17

 Rectangle fault model

1.81 × 1018

6.11

  

 Based on tilt data alone

0.43/1.00

0.46/0.22

 Rectangle fault model

1.07 × 1018

5.95

  
  1. a1 The standard deviation and amount of the slip in the two orthogonal directions (N170E and N80E) at the maximum slip subfault