Ab'/> <![CDATA[Fault dip angle determination with the <ce:inf loc='post'> <ce:bold> <ce:italic>j</ce:italic> </ce:bold> </ce:inf> <ce:bold>?</ce:bold> <ce:inf loc='post'> <ce:bold> <ce:italic>i</ce:italic> </ce:bold> </ce:inf> criterion and coulomb stress changes associated with the 2015 <ce:italic>M <ce:inf loc='post'>w</ce:inf> </ce:italic> 7.9 Gorkha Nepal earthquake revealed by InSAR and GPS data]]>
首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth > j ? i criterion and coulomb stress changes associated with the 2015 M w 7.9 Gorkha Nepal earthquake revealed by InSAR and GPS data]]>
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j ? i criterion and coulomb stress changes associated with the 2015 M w 7.9 Gorkha Nepal earthquake revealed by InSAR and GPS data]]>

机译:<![cdata [cdata [cdata [c cdata [c cdip:inf loc =“post”> j i 标准和库仑压力变化与2015年 m w 7.9 gorkha尼泊尔地震透露,insar和gps数据透露] ]

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AbstractMinimizing data misfit has been widely used in geodetic determination of fault dip angle, however, it ignores the contribution from data noise. Here, we use thej?icriterion, which takes into account both data misfit and the contribution from data noise, to determine dip angle. Synthetic tests show dip angle estimates with thej?icriterion are more accurate and robust than those with data misfit minimization. We applied thisj?icriterion to the determination of the dip angle of the 2015Mw7.9 Gorkha Nepal earthquake using Interferometric Synthetic Aperture Radar (InSAR) and Global Positioning System (GPS) data. The results show that the event ruptured to the north of Kathmandu with a maximum slip value of 5.8m and a dip angle of 9.5°. We also calculated the coulomb failure stress changes resolved onto the receiver faults that are generally consistent with the fault geometry of this event, suggesting the possible triggering relation to aftershocks with low dip angles and a zone of seismic potential located to the west of the rupture zone.展开▼
机译:<![cdata [ 抽象 最小化数据错数已被广泛应用于故障倾角的大地测定,但是,它忽略了数据的贡献噪音。在这里,我们使用 j i 标准,它进入审查数据误操作和数据噪声的贡献,以确定DIP角度。合成测试显示DIP角估计与 j i 标准是比那些具有数据不足最小化的人更准确和强大。我们应用了这个 j i 确定倾角的标准2015年的角度 m w 7.9 gorkha尼泊尔地震使用干涉测量合成孔径雷达(INSAR)和全球定位系统(GPS)数据。结果表明,该事件发生在加德满都北部的最大滑动值5.8米,倾角为9.5°。我们还计算了库仑失败应力变化,这些压力变化在接收器断层上,通常与该事件的故障几何形状一致,表明与具有低汲取角度的余震和位于破裂区域以西的地震潜力区域可能的触发关系。

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