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首页> 外文期刊>Pure and Applied Geophysics >The 8 September 2017 Tsunami Triggered by the M w 8.2 Intraplate Earthquake, Chiapas, Mexico
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The 8 September 2017 Tsunami Triggered by the M w 8.2 Intraplate Earthquake, Chiapas, Mexico

机译:2017年9月8日Tsunami由<重点类型=“斜体”> m <下标> w 8.2 Intraplate地震,恰帕斯,墨西哥

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AbstractThe 8 September 2017,Mw8.2 earthquake offshore Chiapas, Mexico, is the largest earthquake in recorded history in Chiapas since 1902. It caused damage in the states of Oaxaca, Chiapas and Tabasco, including more than 100 fatalities, over 1.5 million people were affected, and 41,000 homes were damaged in the state of Chiapas alone. This earthquake, an intraplate event on a normal fault on the oceanic subducting plate, generated a tsunami recorded at several tide gauge stations in Mexico and on the Pacific Ocean. Here, we report the physical effects of the tsunami on the Chiapas coast and analyze the societal implications of this tsunami on the basis of our post-tsunami field survey. The associated tsunami waves were recorded first at Huatulco tide gauge station at 5:04 (GMT) 12?min after the earthquake. We covered ground observations along 41?km of the coast of Chiapas, encompassing the sites with the highest projected wave heights based on our?preliminary tsunami model (maximum tsunami amplitudes between 94.5° and 93.0°W). Runup and inundation distances were measured along eight sites. The tsunami occurred at low tide. The maximum runup was?~?3?m at Boca del Cielo, and maximum inundation distance was 190?m in Puerto Arista, corresponding to the coast in front of the epicenter and in the central sector of the Gulf of Tehuantepec. Tsunami scour and erosion was evident along the Chiapas coast. Tsunami deposits, mainly sand, reached up to 32?cm thickness thinning landward up to 172?m distance.]]>
机译:<![cdata [ <标题>抽象 ara id =“par1”> 2017年9月8日,<重点类型=“斜体“> M <下标> W 8.2墨西哥地震,是自1902年以来恰帕斯历史上最大的地震中最大的地震。它在瓦哈卡,恰帕斯和塔巴斯科州造成了损害,包括更多100多种死亡人数,超过150万人受到影响,仅在恰帕斯的状态下损坏了41,000所房屋。这种地震,一个关于海洋底板板上正常故障的内部陷阱事件,在墨西哥和太平洋上的几个潮汐量电台上创造了一台Tsunami。在这里,我们报告了海啸海岸海啸的物理效果,并在我们海啸后现场调查的基础上分析了这一海啸的社会影响。相关的海啸波首先在5:04(GMT)12?MIN后首先在Huatulco Tide Cauge站记录。我们沿着恰帕斯的海岸41公里的地面观察,包括基于我们的初步海啸模型(94.5°和93.0°W)的最高投影波高的网站。沿八个站点测量了升空和淹没距离。海啸发生在低潮中。最大的运行次数是?沿着恰帕斯海岸,海啸冲刷和侵蚀是显而易见的。海啸沉积物,主要是沙子,达到32厘米的厚度较薄,距离达到172Ω·米距离。 ]]>

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