Widespread ground motion distribution caused by rupture directivity during the 2015 Gorkha, Nepal earthquake
書誌事項
- 公開日
- 2016-06-23
- 資源種別
- journal article
- 権利情報
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- https://creativecommons.org/licenses/by/4.0
- https://creativecommons.org/licenses/by/4.0
- DOI
-
- 10.1038/srep28536
- 10.60692/2zh2r-9aa83
- 10.60692/2aj18-y8955
- 公開者
- Springer Science and Business Media LLC
説明
<jats:title>Abstract</jats:title><jats:p>The ground motion and damage caused by the 2015 Gorkha, Nepal earthquake can be characterized by their widespread distributions to the east. Evidence from strong ground motions, regional acceleration duration, and teleseismic waveforms indicate that rupture directivity contributed significantly to these distributions. This phenomenon has been thought to occur only if a strike-slip or dip-slip rupture propagates to a site in the along-strike or updip direction, respectively. However, even though the earthquake was a dip-slip faulting event and its source fault strike was nearly eastward, evidence for rupture directivity is found in the eastward direction. Here, we explore the reasons for this apparent inconsistency by performing a joint source inversion of seismic and geodetic datasets, and conducting ground motion simulations. The results indicate that the earthquake occurred on the underthrusting Indian lithosphere, with a low dip angle, and that the fault rupture propagated in the along-strike direction at a velocity just slightly below the <jats:italic>S</jats:italic>-wave velocity. This low dip angle and fast rupture velocity produced rupture directivity in the along-strike direction, which caused widespread ground motion distribution and significant damage extending far eastwards, from central Nepal to Mount Everest.</jats:p>
収録刊行物
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- Scientific Reports
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Scientific Reports 6 (1), 28536-, 2016-06-23
Springer Science and Business Media LLC
- Tweet
キーワード
- Lithosphere
- Ground motion
- Antenna (radio)
- Article
- Directivity
- Engineering
- Seismology
- Civil and Structural Engineering
- High-Resolution Seismic Noise Tomography
- Physics
- Tectonics
- Geology
- FOS: Earth and related environmental sciences
- Subduction
- Computer science
- Seismic Engineering and Ground Motion Analysis
- Earth and Planetary Sciences
- Geophysics
- Seismicity and Tectonic Plate Interactions
- Microseisms
- Physical Sciences
- Slip (aerodynamics)
- Telecommunications
- Peak ground acceleration
- Thermodynamics
- Geodesy
- Aftershock
詳細情報 詳細情報について
-
- CRID
- 1360848658465848832
-
- ISSN
- 20452322
-
- PubMed
- 32332838
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- 資料種別
- journal article
-
- データソース種別
-
- Crossref
- KAKEN
- OpenAIRE

