Table 1 Existing and new deformation rates for the Tuz Gölü Fault Zone

0.04 (northern)

0.053 (southern)

N.D.

Kürçer and Gökten²⁵

Paleoseismic trenching, ¹⁴C and ⁴⁰Ar/³⁹Ar geochronology²³

1.2

4.7

Aktuğ et al.²⁹

Kinematic analysis, GPS block modeling

0.03–0.05 (western)

0.08–0.13 (eastern)

N.D.

Özsayın et al.²¹

Geomorphology, geology, ⁴⁰Ar/³⁹Ar geochronology

N.D.

0.58–3.53

Krystopowicz³⁸

Kinematic analysis and ⁴⁰Ar/³⁹Ar geochronology

0.0714–0.112

N.D.

Öztürk et al.²⁶

Electrical resistivity and thermoluminescence dating,

2.0

1.8

Gezgin et al.³⁰

GNSS, GPS block modeling

N.D.

3

Özbey et al.¹⁷

GPS block modeling, InSAR-kinematic analysis, geomorphology

1.12 ± 0.08^a

same as F3^b

−0.47 ± 0.12^a

same as F3^b

This study

Lava flow F2 restoration and zircon double-dating

0.90 ± 0.06^a

1.23 ± 0.08^b

0.01 ± 0.08^a

0.06 ± 0.08^b

“

Lava flow F3 restoration and zircon double-dating

0.73 ± 0.06^a

1.78 ± 0.08^b

0.30 ± 0.06^a

1.25 ± 0.08^b

“

Lava flow F4 restoration and zircon double-dating