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Table 1. Fault parameters. Latitude and longitude represent vertical projections of the north corner of the upper edge of the fault onto the Earth’s surface. The strike is measured clockwise from the north. The rake is measured on the fault surface counterclockwise from the strike azimuth.

From: Reexamination of the fault slip model of the 1891 M 8.0 Nobi earthquake: The first earthquake detected by a geodetic survey in Japan

Segment

 

Latitude °

Longitude °

Depth km

Width km

Length km

Strike °

Dip °

Rake °

Slip m

1

 

35.9140

136.3630

0.0

15.0

18.0

145.0

90.0

45.0

1.4

2

 

35.7810

136.4770

0.0

15.0

18.0

145.0

90.0

45.0

4.2

Case 1

3

35.6480

136.5910

0.0

15.0

16.0

145.0

90.0

−7.3

7.3

 

4

35.5372

136.7025

0.0

22.5

32.2

114.0

61.5

24.0

2.6

Case 2

3

35.6480

136.5910

0.0

15.0

16.0

145.0

90.0

−8.3

7.5

 

4-1

35.5372

136.7025

0.0

11.2

16.1

114.0

61.5

12.2

3.3

 

4-2

35.4787

136.8648

0.0

11.2

16.1

114.0

61.5

32.8

2.0

 

4-3

35.4930

136.6787

9.9

11.2

16.1

114.0

61.5

2.8

3.8

 

4-4

35.4345

136.8409

9.9

11.2

16.1

114.0

61.5

22.5

3.4