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- W2119133388 abstract "The northern Tehran fault (NTF) is potentially capable of causing large earth-quakes (M max ~ 7.2) in a very densely populated area of northern Tehran, Iran. Due to the lack of recorded strong motion data for earthquakes on the fault, a hybrid simulation method is used to calculate broadband (0.1–20 Hz) ground-motion time histories at bedrock level for deterministic earthquake scenarios on the NTF. Low-frequency components of motion (0.1–1.0 Hz) are calculated using a deterministic approach and the discrete wave number-finite element method in a regional one-dimensional (1-D) velocity model. High frequencies (1.0–20.0 Hz) are calculated by the stochastic finite fault method based on dynamic corner frequency. The results were validated by comparing the simulated peak values and response spectra with the empirical ground motion models available for the area and the Modified Mercalli intensity (MMI) observations from historical earthquakes of the region." @default.
- W2119133388 created "2016-06-24" @default.
- W2119133388 creator A5013028131 @default.
- W2119133388 creator A5034545890 @default.
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- W2119133388 date "2013-05-01" @default.
- W2119133388 modified "2023-10-18" @default.
- W2119133388 title "Prediction of Broadband Ground-Motion Time Histories: The Case of Tehran, Iran" @default.
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- W2119133388 doi "https://doi.org/10.1193/1.4000150" @default.
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