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Slip on the Superstition Hills fault and on nearby faults associated with the 24 November 1987 Elmore Ranch and Superstition Hills earthquakes, southern California

机译:与1987年11月24日在加利福尼亚州南部发生的Elmore Ranch和Superstition Hills地震有关的Superstition Hills断层和附近的断层滑动

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摘要

Alignment arrays and creepmeters spanning several faults in southern California recorded slip associated with the 24 November 1987 Elmore Ranch and Superstition Hills earthquakes. No precursory slip had occurred on the Superstition Hills fault up to 27 October 1987, when the last measurement before the earthquakes was made. About 23 days before the earthquake, dextral creep events of about 13 mm and 0.5 mm may have occurred simultaneously on the Imperial and southern San Andreas faults, respectively, but the tectonic origin of the smaller event is questionable.ududWithin 12 hr after the Superstition Hills earthquake, 20.9 cm of dextral slip occurred on the main fault trace at the Superstition Hills alignment array, and 39.8 cm of dextral slip was recorded over the entire 110-m width of the array. Despite this initial wide distribution of slip, nearly all of the postseismic slip is occurring on the main fault trace. As of 3 August 1988, the alignment array had recorded a total of 80.2 cm of dextral slip. As of 5 days after the earthquakes, 65 to 80 per cent of the total slip measured by the alignment array had occurred on discrete, mappable fractures.ududIn addition, the two earthquakes triggered slip on the Coyote Creek fault, the southern San Andreas fault, and on the Imperial fault. Telemetered data from creepmeters on the southern San Andreas and Imperial faults indicate that triggered slip began there within 3 min or less of each of the two earthquakes. Additional triggered slip occurred on the Imperial fault beginning 3.5 hr after the second earthquake.
机译:横跨加利福尼亚南部几个断层的对准阵列和蠕变仪记录了与1987年11月24日的Elmore Ranch和Superstition Hills地震有关的滑动。直到1987年10月27日,即地震发生前的最后一次测量,在迷信山断裂带上都没有发生先兆滑移。地震发生前约23天,圣安德烈亚斯断层和南部圣安德列斯断层可能分别同时发生了约13mm和0.5mm的右旋蠕变事件,但较小地震的构造起源值得怀疑。 ud ud在Superstition Hills地震中,Superstition Hills对准阵列的主要断层迹线上发生了20.9 cm的右旋滑移,在整个阵列的110 m宽度上记录了39.8 cm的右旋滑移。尽管滑移最初分布广泛,但几乎所有的地震后滑移都发生在主要断层迹线上。到1988年8月3日,对准阵列记录了总共80.2cm的右旋滑移。地震发生5天后,对准阵列测得的总滑移量的65%至80%发生在离散的,可绘制的裂缝上。 ud ud此外,两次地震还触发了位于圣约翰南部的Coyote Creek断层的滑移。安德烈亚斯的错,以及帝国的错。来自南部圣安地列斯和帝国断裂的蠕变仪的遥测数据表明,两次地震中的每一次都在3分钟或更短的时间内触发了滑动。第二次地震发生3.5小时后,在帝国断层上又发生了触发滑移。

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