首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Seismic activity in the Sumatra-Java region prior to the December 26, 2004 (M-W=9.0-9.3) and March 28, 2005 (M-W=8.7) earthquakes
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Seismic activity in the Sumatra-Java region prior to the December 26, 2004 (M-W=9.0-9.3) and March 28, 2005 (M-W=8.7) earthquakes

机译:2004年12月26日(M-W = 9.0-9.3)和2005年3月28日(M-W = 8.7)地震之前在苏门答腊爪哇地区的地震活动

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A promising approach to assessing seismic hazards has been to combine the concept of seismic gaps with Coulomb-stress change modeling to refine short-term earthquake probability estimates. However, in practice the large uncertainties in the seismic histories of most tectonically active regions limit this approach since a stress increase is only important when a fault is already close to failure. In contrast, recent work has suggested that Accelerated Moment Release (AMR) can help to identify when a stretch of fault is approaching failure without any knowledge of the seismic history of the region. AMR can be identified in the regions around the Sumatra Subduction system that must have been stressed before the 26 December 2004 and 28 March 2005 earthquakes. The effect is clearest for the epicentral regions with less than a 2% probability that it could occur in a random catalogue. Less clear AMR is associated with the regions north of Sumatra around the Nicobar and Andaman islands where rupture in the December 2004 earthquake was less vigorous. No AMR is found for the region of the 1833 Sumatran earthquake suggesting that an event in this region in the near future is unlikely. AMR similar to that before the December 2004 and March 2005 events is found for a 750 kin stretch of the southeastern Sumatra and western Java subduction system suggesting that it is close to failure. Should the whole of this stretch break in a single event the magnitude could be similar to the December 2004 earthquake. (c) 2006 Elsevier B.V. All rights reserved.
机译:评估地震危害的一种有前途的方法是将地震缝隙的概念与库仑应力变化模型相结合,以完善短期地震概率估计。但是,实际上,在大多数构造活动区的地震历史中存在很大的不确定性,因此这种方法受到限制,因为应力增加仅在断层已经接近破坏时才重要。相反,最近的工作表明,加速矩释放(AMR)可以在不了解该地区地震历史的情况下,帮助确定断层延伸接近失效的时间。可以在2004年12月26日和2005年3月28日地震之前必须承受压力的苏门答腊俯冲系统周围地区确定AMR。对于震中区域,这种影响最明显,发生在随机目录中的可能性小于2%。不太清楚的AMR与苏门答腊以北尼科巴岛和安达曼群岛周围的地区有关,在2004年12月地震中破裂不那么剧烈。没有发现1833年苏门答腊地震区域的AMR,这表明在不久的将来在该地区发生地震的可能性很小。在东南苏门答腊岛和西爪哇俯冲系统的750 kin延伸中发现了类似于2004年12月和2005年3月事件之前的AMR,表明它已接近失败。如果整个拉伸过程都在一个事件中破裂,则震级可能类似于2004年12月的地震。 (c)2006 Elsevier B.V.保留所有权利。

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