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- W489942576 abstract "Abstract17 August 1999 Gölcük (Kocaeli)-Arifiye (Adapazan) earthquake (Mw=7.4) occurred along the western part of the North Anatolian Fault Zone. The earthquake was centered at 40.702°N, 29.987°E and originated at a depth of 17 km. The earthquake created a 160 km long surface rupture in a right-lateral sense of shear and exhibits two large displacements at two geographic locations that are about 70 km apart. The displacements are 4.1 m at Gölcük and 4.9 m in the south of Arifiye. An inversion analysis of seismic data suggests a two-stage fracturing. 12 November Düzce earthquake (Mw=7.1) occurred to the east of Gölcük-Arifiye line and created a 38 km long surface rupture. The maximum rigth-lateral displacement of 4.5 m occurred in the middle of the surface rupture. To the south of Düzce, the surface ruptures of two earthquakes overlapped by about 10 km length. Düzce earthquake must have been triggered by Gölcük-Arifiye earthquake.KeywordsFracture ZoneSurface RuptureFault Plane SolutionNorth Anatolian FaultCentroid Moment TensorThese keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves." @default.
- W489942576 created "2016-06-24" @default.
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- W489942576 date "2002-01-01" @default.
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- W489942576 title "The 17 August 1999 Gölcük (Kocaelı)- Arıfıye (Adapazari) and 12 November 1999 Düzce Earthquakes, NW Turkey: Their Mechanisms and Tectonic Significance" @default.
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- W489942576 doi "https://doi.org/10.1007/978-94-010-0383-4_1" @default.
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