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Seismicity and Seismotectonics of the Western Lake Ontario Region

机译:西安大略湖地区的地震活动与地震构造

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摘要

The western Lake Ontario region, a traditionally perceived area of low seismic risk, is densely populated and is home to, among other critical facilities, the nuclear reactors of Pickering and Darlington. These and other characteristics of the region call for improved estimates of seismic hazard. Due to a lack of understanding of the causative geological sources and recurrence characteristics of the reported seismic activity, there is considerable uncertainty regarding estimated ground motion parameters, a fundamental component of seismic hazard assessments. To attempt to improve the definition of the seismic source zones and, consequently, seismic hazard assessments, the hypocentres of about 30 local earthquakes were recomputed. A new data compilation, based on the revised locations or those with the least travel-time residuals, shows that local microearthquakes (ML"3.5) generally occur along, or at the intersection of, prominent aeromagnetic or gravity anomalies. A notable seismicity trend extends in a northeast-southwest direction between Toronto and Hamilton, and is bounded by magnetic lineaments. A major geological structure, the Central Metasedimentary Belt Boundary Zone (CMBBZ), coincides with a strong aeromagnetic anomaly which extends to the northeast into the Western Québec Seismic Zone. This magnetic lineament also extends to the south, across Lake Ontario, to join the Akron (Ohio) magnetic boundary that was associated with several historical earthquakes and with a mb=4.9 earthquake in 1986. Most of the seismic events recorded instrumentally in the 20th century have occurred within a depth range of 5 to 20 km. This observation supports the correlation of local earthquakes with deep geophysical and geological features, suggesting contemporary reactivation of basement structures. This may imply that a more conservative deterministic hazard estimate is needed to verify the probabilistic approach currently used to assess seismic hazard in southern Ontario.
机译:安大略湖西部地区是传统上公认的地震风险低的地区,人口稠密,除其他重要设施外,还拥有Pickering和Darlington核反应堆。该地区的这些和其他特征要求对地震危险性进行改进的估算。由于缺乏对所报告地震活动的成因地质源和复发特征的了解,因此有关估计的地震动参数(地震危险性评估的基本组成部分)存在很大的不确定性。为了改善对震源区的定义,进而改善对地震的危害性评估,重新计算了大约30次局部地震的震中。根据修订后的位置或旅行时间残差最少的位置进行的新数据汇编显示,局部微地震(ML“ 3.5)通常发生在显着的航磁或重力异常的沿或相交处。地磁沉积带边界带(CMBBZ)是一个主要的地质构造,与一个强烈的航磁异常相吻合,从东北向西延伸到魁北克西部地震带,地处多伦多和汉密尔顿之间的东西-西南方向。 。这种磁线也延伸到南部,横跨安大略湖,与阿克伦(俄亥俄州)的磁边界合并,该磁边界与几次历史性地震以及1986年的mb = 4.9地震有关。一个世纪发生在5至20 km的深度范围内,这一观察结果支持了当地地震与深部地球物理和地质现象的相关性。的生物学特征,暗示了地下室结构的当代复兴。这可能意味着需要更保守的确定性灾害估计,以验证当前用于评估安大略南部地震灾害的概率方法。

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    Mohajer Arsalan A.;

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  • 年度 1993
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