Tectonic Geomorphological Active Fault Studies in Japan after 1980

IF 0.3 Q4 GEOGRAPHY, PHYSICAL
Suzuki Yasuhiro
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引用次数: 6

Abstract

Tectonic geomorphology has played important roles in active fault studies in Japan. Following large historical earthquakes, the concept of active fault was formulated and detailed information has rapidly accumulated. This paper reviews the progress of active fault studies in Japan since the 1980s. The period 1980 to 1994 can be regarded as the matured period of active fault studies during seismic calm. The studies conducted during this period are categorized into the following: 1) excavation studies of active faults, 2) analytical studies of tectonic landform evolution based on dislocation models, 3) chronological studies supported by the development of age determination techniques, and 4) studies quantifying the rate of crustal deformation. In 1995, the Great Kobe Earthquake occurred. The earthquake triggered a seismically active period in Japan, and the active fault has become an important issue in disaster mitigation. The research in the decade after 1995 can be summarized as follows: 1) intensive investigations of active faults, 2) detailed large-scale mapping, 3) seismic reflection profiling, 4) long-term forecasts of earthquakes, 5) careful study of flexural deformation, and 6) overseas research on large destructive earthquakes. Then, the period since 2005 has witnessed the rediscovery of active faults, with research considering 1) the relations between the large earthquakes which often occurred in this period and their seismogenic active faults, 2) precise distribution of active faults, 3) the relations between active tectonics and geodetical movement, 4) the relations between interplate earthquakes and submarine active faults, and 5) the difficult problems of prevention against infrequent disasters like the 2011 Great East Japan Earthquake. Additionally, since around 2006, some nuclear power plants have faced problems associated with active faults because some active faults had been overlooked or ignored in the seismic design of these plants. Active fault research now bears greater social responsibility.
1980年后日本构造地貌活动断层研究
构造地貌学在日本的活动断层研究中占有重要地位。随着历史大地震的发生,活动断层的概念逐渐形成,详细的资料也迅速积累起来。本文综述了20世纪80年代以来日本活动断层研究的进展。1980 ~ 1994年是地震平静期活动断层研究的成熟期。在此期间开展的研究主要包括:1)活动断层的开挖研究;2)基于位错模型的构造地貌演化分析研究;3)以年龄测定技术为支撑的年代学研究;4)量化地壳变形速率的研究。1995年,发生了神户大地震。地震引发了日本的地震活跃期,活动断层已成为减灾中的一个重要问题。1995年以后10年的研究可以概括为:1)活动断层的深入研究;2)详细的大尺度制图;3)地震反射剖面;4)地震的长期预报;5)弯曲变形的认真研究;6)国外对大破坏性地震的研究。2005年以来,活动性断裂再次被发现,研究考虑了1)这一时期频繁发生的大地震与其发震活动断裂的关系,2)活动断裂的精确分布,3)活动构造与大地运动的关系,4)板块间地震与海底活动断裂的关系,5)预防罕见灾害(如2011年东日本大地震)的难题。此外,自2006年左右以来,一些核电站面临着与活动断层有关的问题,因为一些活动断层在这些核电站的抗震设计中被忽视或忽略了。活动断层研究现在承担着更大的社会责任。
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CiteScore
1.50
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0.00%
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4
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