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Using new models to assess probabilistic seismic hazard of the North-South Seismic Zone in China

机译:使用新模型评估中国南北地震带的概率地震危险

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The North-South Seismic Zone is a well-known seismotectonic zone in China that frequently experiences major earthquakes. A new probabilistic seismic hazard assessment (PSHA) for this zone is required. In this study, we perform a new PSHA for the North-South Seismic Zone with new models, including a fault source model and a time-dependent seismicity model of major-earthquake seismogenic structures. We demonstrate that the seismic hazard in areas near faults calculated using the fault source model is higher than that calculated using the area model. Faults close to their expected recurrence time for major earthquakes have high seismic hazard. Areas of high seismic hazard in the North-South Seismic Zone between 2016 and 2065 are the Moxi Segment of the Xianshuihe Fault, the Anninghe Fault, and the Daliangshan Fault. High-seismic-hazard areas between 2066 and 2115 are the Luhuo and Zheduotang segments of the Xianshuihe Fault and the Anninghe Fault. The Moxi Segment of the Xianshuihe Fault has the highest seismic hazard over the next 50 years.
机译:南北地震带是中国著名的地震构造带,经常发生大地震。需要对该区域进行新的概率地震危险性评估(PSHA)。在这项研究中,我们使用新模型对南北地震带进行了新的PSHA,包括断层震源模型和大地震发震结构的时变地震模型。我们证明,使用断层源模型计算的断层附近区域的地震危险性高于使用区域模型计算的区域。接近大地震预期复发时间的断层具有很高的地震危险性。 2016年至2065年南北地震带中地震危险性较高的地区是咸水河断裂,安宁河断裂和大山山断裂的磨溪段。 2066年至2115年之间的高地震危险区是咸水河断裂带和安宁河断裂带的卢霍和哲多塘段。未来50年内,咸水河断裂的磨溪段地震危险性最高。

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