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首页> 外文期刊>Proceedings of the Geologists' Association >Misattributed tsunami 4: the 2014.04.01 Iquique (Chile) M-w 8.2 earthquake
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Misattributed tsunami 4: the 2014.04.01 Iquique (Chile) M-w 8.2 earthquake

机译:错误归类的海啸4:2014.04.01伊基克(智利)慕尼黑8.2级地震

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The recurring mismatch between the magnitude of subduction earthquakes and related tsunamis hinders hazard assessment. A tsunami which accompanied the 2014.04.01 M-w 8.2 Iquique earthquake and attained <= 2.11 m on the north Chilean coast is generally attributed to slip at a depth of 23 km on the megathrust between the Nazca and South American plates but, as at some other such sites, elastic seafloor deformation resulting from interplate displacements may have been supplemented if not overshadowed as the primary tsunamigenic agent by upper plate faulting. The evidence for suitable structures includes foreshocks M <= 5.8 dating from the preceding month and, during the 24 h immediately after the main shock, aftershocks M <= 5.6. (C) 2015 The Geologists' Association. Published by Elsevier Ltd. All rights reserved.
机译:俯冲地震和相关海啸之间反复发生的不匹配阻碍了危害评估。伴随2014.04.01 Mw 8.2伊基克地震发生的海啸,在智利北部沿海 2.11 m,通常被归因于纳斯卡和南美板块之间的超大推力滑动了23 km的深度,但在其他一些地方在这些部位,由于板间位移而引起的弹性海底变形可能已经被补充,即使没有被上板断裂作为主要的海啸成因剂所掩盖。合适结构的证据包括从上个月开始的前震M <= 5.8,在主震发生后的24小时内,余震M <= 5.6。 (C)2015年地质学家协会。由Elsevier Ltd.出版。保留所有权利。

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