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Seismotectonic-Geologic Hazards Zoning of Iran

机译:伊朗地震构造地质灾害分区

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Seismotectonic-geologic hazards zoning map of Iran is drawn based on deterministic seismic hazards evaluation using the seismicity records, structural trends, tectonic settings, fault ruptures and neotectonics activities in Iran. This map has been prepared to indicate the seismotectonic-geologic hazards of Iran. It contains the earthquake hazards parameters such as b value and Mmax for the nineteen seismotectonic provinces. Furthermore, Moho discontinuity depth, seismogenic layer depths and seismic rates for all provinces are investigated. The majority of deformation in Iran has been concentrated in the continental crust of the country. Zagros and Alborz experience deep earthquakes that are an indication of existence of the thick-skinned tectonics. Finally, some provinces such as Piranshahr- Borojen, East Iran, Naien- Rafsanjan and East Alborz, which include main suture zones of Iran, have faced high seismic hazards.
机译:基于确定性地震危险性评估,使用伊朗的地震记录,结构趋势,构造环境,断层破裂和新构造活动,绘制了伊朗的地震构造地质灾害分区图。该地图已经准备好显示伊朗的地震构造地质灾害。它包含19个地震构造省份的地震灾害参数,例如b值和Mmax。此外,还研究了所有省份的莫霍面不连续深度,发震层深度和地震发生率。伊朗的大部分变形都集中在该国的大陆壳上。扎格罗斯(Zagros)和阿尔伯兹(Alborz)经历了深层地震,这表明存在厚皮层构造。最后,包括伊朗主要缝合区在内的一些省份,例如Piranshahr-Borojen,伊朗东部,Naien-Rafsanjan和East Alborz,都面临着很高的地震危险。

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