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Stopping phase reveals abrupt arrest of large strike-slip earthquakes Í£Ö¹Ïà½Òʾ´óÐÍ×ß»¬µØÕðµÄͻȻֹÁÑ ¡ø ×÷ÕߣºJESSE KEARSE AND YOSHIHIRO KANEKO ¡øÁ´½Ó£º https://www.science.org/doi/10.1126/science.aef3733 ¡øÕªÒª£º µØÕðÕð¼¶ÊÜ¿ØÓÚÆÆÁÑ´«²¥Ôںδ¦¡¢ºÎʱֹͣ¡£È»¶ø£¬ÔÚÌìÈ»µØÕðµÄ½ü³¡µØÕð¼Ç¼ÖУ¬ÆÆÁÑÖ¹ÁÑÏÖÏóºÜÉÙ±»Ö±½Ó¹Û²âµ½¡£Ñо¿ÕßչʾÁË´óÐÍ×ß»¬µØÕðÖеØÃæÔ˶¯Í£Ö¹ÏàµÄϵͳÐÔ½ü³¡¹Û²â½á¹û¡£¶ÔÈ«Çò12´ÎµØÕðʼþµÄ·ÖÎö±íÃ÷£¬Æ½Ðжϲ㷽ÏòµÄµØ±íÎ»ÒÆÖеÄ˲̬¹ý³åÊÇÆÆÁÑ´«²¥Í»È»ÖÕÖ¹µÄ¿É¿¿Õï¶Ï±êÖ¾¡£ ¶¯Ì¬ÆÆÁÑÄ£ÄâÏÔʾ£¬Ç³²ãµÍ²¨ËÙÑÒʯ»áÇ¿ÁÒ·Å´ó½ü³¡µØ¶¯Ðźţ¬´Ó¶øÔöÇ¿µØ±í¼Ç¼µ½µÄÎ»ÒÆ¹ý³å·ù¶È¡£Í£Ö¹Ïà³öÏÖÔÚÔ¶ÀëÒÑÖªÆÆÁÑÄ©¶ËµÄ½ü¶Ï²ãλÖã¬ÕâÒâζ×Å´óÐÍ×ß»¬µØÕðÒԷֶη½Ê½ÆÆÁÑ£¬¶¯Ì¬ÆÆÁÑ´«²¥ÔÚÄÚ²¿¶Ï²ã¶Î±ß½ç´¦»á±»Í»È»ÖÐÖ¹²¢ÖØÐÂÆô¶¯¡£ ¡ø Abstract£º Earthquake magnitude is controlled by where and when rupture propagation stops. However, rupture arrest has rarely been directly observed in near-field seismic records of natural earthquakes. Here, we present systematic near-field observations of ground-motion stopping phases from large strike-slip earthquakes. Analysis of 12 global events shows that transient overshoot in fault-parallel ground surface displacement is a robust diagnostic signature of abrupt termination of rupture propagation. Dynamic rupture simulations reveal that near-field ground motions are strongly amplified by low-wavespeed rocks at shallow depth, which enhances the amplitude of displacement overshoot recorded at the surface. The occurrence of stopping phases at near-fault locations far from mapped rupture termini implies that large strike-slip earthquakes rupture in a segmented manner, with dynamic rupture propagation punctuated by abrupt arrest and reinitiation at internal fault-segment boundaries. |
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