首页> 外文期刊>Bulletin of the Seismological Society of America >Step-Over and Bend Structures along the 1999 Duzce Earthquake Surface Rupture, North Anatolian Fault, Turkey
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Step-Over and Bend Structures along the 1999 Duzce Earthquake Surface Rupture, North Anatolian Fault, Turkey

机译:土耳其北安纳托利亚断层1999年杜兹地震地表破裂的越过和弯曲结构

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摘要

The 12 November 1999 Duzce earthquake (Mw 7.1), which occurred on the Duzce fault of the North Anatolian Fault Zone, formed a 40-km-long surface rupture, which extended between Golyaka in the west and Kaynasli in the east. The earthquake nucleated close to the Beykoy step-over, a 0.8-km-wide and 1.8-km-long pressure ridge, with bilateral rupture propagation both to the west and the east. The Beykoy, Kaynasli, and Cevizlik step-overs, through which the 1999 Duzce rupture propagated, are less than 2.5 km wide. The Eften and Bakacak step-overs, where the rupture was arrested, are more than 4 km wide. These exceptional dimensions of step-overs associated with the 1999 Duzce rupture were investigated for their influence on rupture propagation.
机译:1999年11月12日在北安那托利亚断层带的杜兹断层上发生的 地震(M w 7.1)形成了一个40-公里长的表面破裂,在西部的Golyaka 和东部的Kaynasli之间延伸。地震成核后靠近贝科伊(Beykoy)阶跃的 ,宽为0.8公里,长为1.8公里的 压力脊,双侧破裂都传播到了 西方和东方。通过 传播的Beykoy,Kaynasli和Cevizlik阶跃跨度小于2.5 km ,1999年Duzce破裂传播了此阶跃。破裂被 阻止的Eften和Bakacak过渡段的宽度超过4 km。研究了与1999年Duzce破裂有关的阶跃的这些特殊尺寸 对破裂传播的影响。

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