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• W2559533561 abstract "Along the North Anatolian fault (NAF), the surface deformation associated with tectonic block motions, elastic strain accumulation, and the viscoelastic response to past earthquakes has been geodetically observed over the last two decades. These observations include campaign‐mode Global Positioning System (GPS) velocities from the decade prior to the 1999 M w 7.4 Izmit earthquake and seven years of continuously recorded postseismic deformation following the seismic event. Here, we develop a 3D viscoelastic block model of the greater NAF region, including the last 2000 yrs of earthquake history across Anatolia, to simultaneously explain geodetic observations from both before and after the Izmit earthquake. With a phenomenologically motivated simple two‐layer structure (schizosphere and plastosphere) and a Burgers rheology (with Maxwell viscosity log10 η M≈18.6–19.0  Pa·s and Kelvin viscosity log10 η K≈18.0–19.0  Pa·s), a block model that incorporates tectonic plate motions, interseismic elastic strain accumulation, transient viscoelastic perturbations, and internal strain can explain both the pre‐ and post‐Izmit earthquake observations with a single unified model. Viscoelastic corrections to the interseismic GPS velocity field with the unified model reach magnitudes of ∼2.9  mm/yr. Geodetically constrained slip‐deficit rate estimates along the central NAF and northern strand of the NAF in the Sea of Marmara vary nonmonotonically with Maxwell viscosity and change by up to 23% (∼4  mm/yr) for viscosities ranging from 1018 to 1023  Pa·s. For the best‐fit viscosity structures, central NAF slip‐deficit rates reach 22  mm/yr, increasing to 28  mm/yr in the Sea of Marmara. Along the central NAF, these rates are similar to the fastest geologic slip‐rate estimates. The fastest slip‐deficit rate estimates along the entire fault system (∼27–28  mm/yr) occur less than 50 km from Istanbul, along the northern strand of the NAF in the Sea of Marmara.[Electronic Supplement:][1] Figure of sensitivity of viscoelastic block model slip‐deficit rate estimates and contour plot of mean residual improvement. [1]: http://www.bssaonline.org/lookup/suppl/doi:10.1785/0120160120/DOIsuffix/-/DC1" @default.
• W2559533561 created "2016-12-08" @default.
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• W2559533561 date "2016-11-29" @default.
• W2559533561 modified "2023-09-26" @default.
• W2559533561 title "Viscoelastic Block Models of the North Anatolian Fault: A Unified Earthquake Cycle Representation of Pre‐ and Postseismic Geodetic Observations" @default.
• W2559533561 cites W1487214760 @default.
• W2559533561 cites W1489937293 @default.
• W2559533561 cites W1491417518 @default.
• W2559533561 cites W1521790884 @default.
• W2559533561 cites W1538087140 @default.
• W2559533561 cites W1600960604 @default.
• W2559533561 cites W1658186794 @default.
• W2559533561 cites W1876019606 @default.
• W2559533561 cites W1895442870 @default.
• W2559533561 cites W1963569243 @default.
• W2559533561 cites W1967488184 @default.
• W2559533561 cites W1968606632 @default.
• W2559533561 cites W1969168621 @default.
• W2559533561 cites W1974932270 @default.
• W2559533561 cites W1979255487 @default.
• W2559533561 cites W1981165981 @default.
• W2559533561 cites W1981370501 @default.
• W2559533561 cites W1984459965 @default.
• W2559533561 cites W1992428966 @default.
• W2559533561 cites W1993182720 @default.
• W2559533561 cites W2011078679 @default.
• W2559533561 cites W2016489368 @default.
• W2559533561 cites W2023558112 @default.
• W2559533561 cites W2023571756 @default.
• W2559533561 cites W2023815011 @default.
• W2559533561 cites W2024301974 @default.
• W2559533561 cites W2039280992 @default.
• W2559533561 cites W2045005419 @default.
• W2559533561 cites W2046584974 @default.
• W2559533561 cites W2047080222 @default.
• W2559533561 cites W2068176534 @default.
• W2559533561 cites W2068985200 @default.
• W2559533561 cites W2077313228 @default.
• W2559533561 cites W2082712001 @default.
• W2559533561 cites W2082728801 @default.
• W2559533561 cites W2087058805 @default.
• W2559533561 cites W2095619349 @default.
• W2559533561 cites W2100074656 @default.
• W2559533561 cites W2105384397 @default.
• W2559533561 cites W2111061528 @default.
• W2559533561 cites W2111826571 @default.
• W2559533561 cites W2112876739 @default.
• W2559533561 cites W2119117154 @default.
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• W2559533561 cites W2125364013 @default.
• W2559533561 cites W2125671949 @default.
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• W2559533561 cites W2135607818 @default.
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• W2559533561 doi "https://doi.org/10.1785/0120160059" @default.
• W2559533561 hasPublicationYear "2016" @default.
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