Kamchatka subduction zone, May 2013: the Mw 8.3 deep earthquake, preceding shallow swarm and numerous deep aftershocks

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• 作者：Ale? ?pi?ák (1)
  Ji?í Vaněk (1)
  
• 关键词：Kamchatka ; deep earthquake ; earthquake swarm ; Wadati ; Benioff zone
• 刊名：Studia Geophysica et Geodaetica
• 出版年：2014
• 出版时间：January 2014
• 年：2014
• 卷：58
• 期：1
• 页码：76-83
• 全文大小：1,143 KB
• 作者单位：Ale? ?pi?ák (1)
  Ji?í Vaněk (1)
  
  1. Institute of Geophysics, Academy of Sciences of the Czech Republic, Bo?ní II/1401, 141 31, Praha 4, Czech Republic
  
• ISSN：1573-1626

文摘

A sequence of 98 teleseismically recorded earthquakes occurred off the east coast of Kamchatka at depths between 10-90 km around latitude 52.5°N and longitude 160°E on May 16-3, 2013. The swarm occurred along the northern limit of the rupture area of the 1952 Mw 9.0 great Kamchatka earthquake, the fifth largest earthquake in the history of seismic observations. On May 24, 2013 the strongest deep earthquake ever recorded of Mw 8.3 occurred beneath the Sea of Okhotsk at a depth of 610 km in the Pacific slab of the Kamchatka subduction zone, becoming the northernmost deep earthquake in the region. The deep Mw 8.3 earthquake occurred down-dip of the shallow swarm in a transition zone between the southern deep and northern shallow segments of the Pacific slab. Several deep aftershocks followed, covering a large, laterally elongated part of the slab. We suppose that the two described earthquake sequences, the May 16-3 shallow earthquake swarm and the May 24-8 deep mainshock-aftershock series, represent a single tectonic event in the Pacific slab having distinct properties at different depth levels. A low-angle underthrusting of the shallow part of the slab recorded by the shallow earthquake swarm activated the deep part; this process induced the deep mainshock-aftershock series only three days after the swarm. The domain of the subducting slab activated by the May 2013 earthquake occurrence was extraordinarily large both down-dip and along-strike.