Pure dip-slip along the Tuz Gölü Fault Zone accommodates east-west extension of Central Anatolia
Kinematic constraints on faults with slow slip rates often diverge, obscuring their neotectonic significance and seismic hazards. The Tuz Gölü Fault Zone (TGFZ) is a major slow-moving fault accommodating intraplate deformation within Central Anatolia, for which long-term geological and short-term...
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| Hauptverfasser: | , , , , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
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30 April 2025
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| In: |
Communications earth & environment
Year: 2025, Jahrgang: 6, Heft: 1, Pages: 1-12 |
| ISSN: | 2662-4435 |
| DOI: | 10.1038/s43247-025-02192-6 |
| Online-Zugang: | Verlag, kostenfrei, Volltext: https://doi.org/10.1038/s43247-025-02192-6 Verlag, kostenfrei, Volltext: https://www.nature.com/articles/s43247-025-02192-6 
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| Verfasserangaben: | Gülin Gençoğlu Korkmaz, Janet C. Harvey, Martin Danišík, Lindsay M. Schoenbohm & Axel K. Schmitt |
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| 520 | |a Kinematic constraints on faults with slow slip rates often diverge, obscuring their neotectonic significance and seismic hazards. The Tuz Gölü Fault Zone (TGFZ) is a major slow-moving fault accommodating intraplate deformation within Central Anatolia, for which long-term geological and short-term geodetic deformation rates disagree. Here, the Pleistocene-Recent kinematic evolution of the TGFZ is determined by dating dissected lava flows of the Hasandağ stratocone. Combined zircon U-Th and (U-Th)/He ages indicate emplacement between 151 ± 6 ka and 38.8 ± 2.0 ka (2σ uncertainties). Restoring flow levees as tie points across fault scarps yields vertical displacement rates of 0.90 ± 0.06 to 1.23 ± 0.08 mm/a for the most reliable projections, whereas in contrast to previous notions only negligible dextral strike slip at 0.01 ± 0.08 to 0.06 ± 0.08 mm/a is permitted. Predominantly normal faulting without a major strike-slip component for the TGFZ supports ongoing east-west extension without the requirement for shearing due to north-south shortening of Central Anatolia between its bounding megashears as it gradually escapes westward. | ||
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