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A re-examination of historic earthquakes in the San Jacinto fault zone, California

机译:重新检查加利福尼亚州圣哈辛托断裂带的历史地震

摘要

The high level of seismic activity and the potential for large earthquakes in the San Jacinto fault zone, southern California, make it desirable to have accurate locations and source parameters for as many previous events as possible. Prior to the installation of a dense seismic network in this region, earthquakes were located using only a few stations with generally poor azimuthal coverage resulting in considerable uncertainty in the locations. We relocate and obtain moment estimates for historic (pre-WWSSN) earthquakes in the western Imperial Valley by comparing the waveforms and travel times with recent earthquakes in the region. All the events are in the M_L 5.5 to 6.5 range. The historic earthquakes of interest occurred in 1937, 1942, and 1954. We use the 1968 Borrego Mountain, 1969 Coyote Mountain, and 1987 Elmore Ranch earthquakes as calibration events. We employ regional and teleseismic data from continuously operating stations, with Pasadena, DeBilt, Berkeley, Ottawa, and St. Louis recording most of the events. The waveforms imply that all the events are almost pure strike-slip events on vertical or near-vertical faults. Approximate values for the strikes were obtained and are within the range of observed strikes for well-studied earthquakes in this region. The earthquakes are relocated by comparing S-P and surface-wave - S travel times of historic events with the presumably well-located recent events. The relocations require only a small change in location for the 1954 event and a larger adjustment in the 1942 epicenter. It also appears that the 1969 earthquake may have been mislocated. The moment estimates are obtained by direct comparison of the maximum amplitudes. The moment estimates imply that the 1968 and not the 1942 earthquake is the largest to have occurred in the region this century. Previous magnitude estimates suggested the 1942 event was larger.
机译:加利福尼亚南部圣哈辛托断裂带的高水平地震活动和大地震的可能性使人们希望对尽可能多的先前事件具有准确的位置和震源参数。在该地区安装密集的地震网络之前,仅使用少数几个方位角覆盖范围较广的站点进行地震定位,从而导致位置的不确定性。通过将波形和传播时间与该地区最近的地震相比较,我们重新定位并获得了帝国西部西部历史性(WWSSN之前)地震的矩估计。所有事件均在M_L 5.5至6.5范围内。感兴趣的历史性地震发生在1937年,1942年和1954年。我们使用1968年的Borrego山,1969年的Coyote山和1987年的Elmore Ranch地震作为校准事件。我们使用来自连续运行站的区域和远程地震数据,其中帕萨迪纳(Pasadena),德比尔特(DeBilt),伯克利(Berkeley),渥太华(Ottawa)和圣路易斯(St. Louis)记录了大部分事件。波形表明,所有事件几乎都是垂直或近垂直断层上的纯走滑事件。获得了该走向的近似值,并且在对该区域进行了充分研究的地震的观测走向范围内。通过比较历史事件的S-P和表面波-S的传播时间与大概位置良好的近期事件,地震得以重新定位。对于1954年的事件,搬迁仅需要更改位置,并在1942年的震中进行较大的调整。看来1969年地震可能已错位。力矩估计值是通过直接比较最大振幅获得的。目前的估计表明,1968年而不是1942年的地震是本世纪该地区发生的最大地震。先前的震级估计表明1942年的事件规模更大。

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