• <tr id="yyy80"></tr>
  • <sup id="yyy80"></sup>
  • <tfoot id="yyy80"><noscript id="yyy80"></noscript></tfoot>
  • 99热精品在线国产_美女午夜性视频免费_国产精品国产高清国产av_av欧美777_自拍偷自拍亚洲精品老妇_亚洲熟女精品中文字幕_www日本黄色视频网_国产精品野战在线观看 ?

    A large aftershock of the 2008 Sichuan earthquake(M W=7.9)triggered by shear waves reflected from the earth core

    2010-04-05 03:36:01ChengHorngin林正洪andWenYenChang
    地震科學(xué)進(jìn)展 2010年6期

    Cheng-Horng L in(林正洪)and Wen-Yen Chang

    1)Institute of Earth Sciences,Academia Sinica,Taipei 115 2)Science Council,Taipei 106

    Since the Earth outer core is liquid,the shear waves that are generated by a large earthquake and traveling to the co re(ScS)will totally reflect with strong seismic energy.It is interesting to note that one large aftershock(MW=6.0)of the 2008 Sichuan earthquake(MW=7.9)in China just occurred when the ScS phase returned around 15.5 minutes later after the mainshock occurred.The estimated peak dynamic stress(~3.3 kPa)of the ScS amplitude was reaching to the generally lower bound for capable of triggering earthquakes.Both the temporal correlation between the aftershock occurrence and the ScS arrival as well as the large enough dynamic stress suggest that the largest aftershock might be triggered dynamically by the ScS waves.Further statistic examinations of 24 major earthquakes(MW>7.5)since 2000 show some large aftershocks(MW>5.0)also coincidentally occurred around the ScS phase arrived.Those observations imp ly that aftershocks might likely be triggered dynamically by the ScS phases,and thus a tempo ralwarning for potentially destructive aftershocks might be considered in the future great earthquakes.

    金乡县| 灯塔市| 汤阴县| 安国市| 金坛市| 冀州市| 丹凤县| 洛南县| 元氏县| 旌德县| 水富县| 孙吴县| 连州市| 富宁县| 肃北| 博客| 海安县| 莒南县| 桂林市| 剑川县| 昌都县| 长顺县| 石阡县| 福泉市| 荥经县| 丘北县| 横峰县| 漳浦县| 海丰县| 谷城县| 永兴县| 绥阳县| 荥阳市| 辽阳县| 北碚区| 闽侯县| 渝北区| 九江县| 玉门市| 荆州市| 东光县|