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- W2797335956 abstract "Earthquakes are caused by the release of tectonic strain accumulated between events. Recent advances in satellite geodesy mean we can now measure this interseismic strain accumulation with a high degree of accuracy. But it remains unclear how to interpret short-term geodetic observations, measured over decades, when estimating the seismic hazard of faults accumulating strain over centuries. Here, we show that strain accumulation rates calculated from geodetic measurements around a major transform fault are constant for its entire 250-year interseismic period, except in the ~10 years following an earthquake. The shear strain rate history requires a weak fault zone embedded within a strong lower crust with viscosity greater than ~1020 Pa s. The results support the notion that short-term geodetic observations can directly contribute to long-term seismic hazard assessment and suggest that lower-crustal viscosities derived from postseismic studies are not representative of the lower crust at all spatial and temporal scales." @default.
- W2797335956 created "2018-04-24" @default.
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- W2797335956 date "2018-04-11" @default.
- W2797335956 modified "2023-10-14" @default.
- W2797335956 title "Constant strain accumulation rate between major earthquakes on the North Anatolian Fault" @default.
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- W2797335956 doi "https://doi.org/10.1038/s41467-018-03739-2" @default.
- W2797335956 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/5895838" @default.
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