Geological and historical evidence of irregular recurrent earthquakes in Japan

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Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/103645

Title:	Geological and historical evidence of irregular recurrent earthquakes in Japan
Authors:	佐竹健治;Satake, Kenji
Contributors:	地球科學學院地球科學學系
Keywords:	Characteristic Earthquake Model;Earthquake;Palaeoseismology;Recurrence Interval;Subduction Zones;Tsunami
Date:	2015-10-28
Issue Date:	2026-04-23 11:34:30 (UTC+8)
Publisher:	The Royal Society;England: The Royal Society
Abstract:	摘要： Great (M∼8) earthquakes repeatedly occur along the subduction zones around Japan and cause fault slip of a few to several metres releasing strains accumulated from decades to centuries of plate motions. Assuming a simple ‘characteristic earthquake’ model that similar earthquakes repeat at regular intervals, probabilities of future earthquake occurrence have been calculated by a government committee. However, recent studies on past earthquakes including geological traces from giant (M∼9) earthquakes indicate a variety of size and recurrence interval of interplate earthquakes. Along the Kuril Trench off Hokkaido, limited historical records indicate that average recurrence interval of great earthquakes is approximately 100 years, but the tsunami deposits show that giant earthquakes occurred at a much longer interval of approximately 400 years. Along the Japan Trench off northern Honshu, recurrence of giant earthquakes similar to the 2011 Tohoku earthquake with an interval of approximately 600 years is inferred from historical records and tsunami deposits. Along the Sagami Trough near Tokyo, two types of Kanto earthquakes with recurrence interval of a few hundred years and a few thousand years had been recognized, but studies show that the recent three Kanto earthquakes had different source extents. Along the Nankai Trough off western Japan, recurrence of great earthquakes with an interval of approximately 100 years has been identified from historical literature, but tsunami deposits indicate that the sizes of the recurrent earthquakes are variable. Such variability makes it difficult to apply a simple ‘characteristic earthquake’ model for the long-term forecast, and several attempts such as use of geological data for the evaluation of future earthquake probabilities or the estimation of maximum earthquake size in each subduction zone are being conducted by government committees. 其他題名： Phil. Trans. R. Soc. A 其他題名： Philos Trans A Math Phys Eng Sci 出版者： England: The Royal Society 出版日期： 2015-10-28 出處： Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 2015-10, Vol.373 (2053), p.20 資源來源： JSTOR Life Sciences Collection 版權： 2015 The Author(s) 版權： 2015 The Author(s). 識別號： ISSN: 1364-503X 識別號： EISSN: 1471-2962 識別號： DOI: 10.1098/rsta.2014.0375 識別號： PMID: 26392616
Appears in Collections:	[Department of Earth Sciences ] journal & Dissertation

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