Skip to main content

Table 5 Results for the data set from the examined fault scarps in western Anatolia

From: Seismic history of western Anatolia during the last 16 kyr determined by cosmogenic 36Cl dating

Graben/

Fault

Number of events

Beginning of 36Cl accumulation (ka)

Age (ka)

Slip per event (m)

Incremental slip rate (mm/yr)

Average slip rate (mm/yr)

Potential Magnitude based on fault length

Calculated magnitude based on modeled slip

Gediz-AlaÅŸehir graben

Rahmiye

3

47

12.0 ± 3.0

8.9 ± 2.2

4.2 ± 1.0

2.0 ± 0.3

0.9 ± 0.1

3.3 ± 0.5

0.6

0.2

0.7

0.5

6.9–7.0

6.6–7.0

Mugırtepe

1

27

6.5 ± 1.6

2.7 ± 0.4

 > 0.3

0.3

6.9

6.9

Manastır

2

9

3.5 ± 0.9

2.0 ± 0.5

3.3 ± 0.5

3.6 ± 0.5

 > 2.2

1.8

1.9

6.9

7.0

Büyük Menderes graben

Kalafat

3

22

15.3 ± 3.8

8.4 ± 2.1

3.6 ± 0.9

0.7 ± 0.1

0.9 ± 0.1

3.1 ± 0.5

 > 0.1

0.2

0.9

0.3

6.4–6.5

6.5–7.0

Yavansu

3

12

7.9 ± 2.0

3.4 ± 0.8

2.0 ± 0.5

0.6 ± 0.1

3.5 ± 0.5

2.6 ± 0.4

 > 0.1

1.7

0.9

0.6

6.7

6.5–7.0

Priene-Sazlı

4

21

8.1 ± 2.0

6.0 ± 1.5

3.7 ± 0.9

2.2 ± 0.5

3.4 ± 0.5

1.5 ± 0.2

1.4 ± 0.2

1.5 ± 0.2

 > 1.3

0.5

0.7

0.5

0.8

6.9

6.7–7.0

Gökova graben

Ören

4

25

8.5 ± 2.0

6.0 ± 1.5

4.3 ± 1.0

1.9 ± 0.5

3.4 ± 0.5

4.2 ± 0.6

2.3 ± 0.3

1.8 ± 0.3

1.2

2.1

0.8

0.8

1.2

7.3–7.5

6.8–7.1