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首页> 外文期刊>Annals Of Geophysics >GPS observations of coseismic?deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central?Italy): data, analysis and preliminary fault model
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GPS observations of coseismic?deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central?Italy): data, analysis and preliminary fault model

机译:2016年8月24日Mw 6阿马里切特地震(意大利中部)的同震变形的GPS观测:数据,分析和初步断层模型

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We used continuous Global Positioning System (GPS) measurements to infer the fault geometry and the amount of coseismic slip associated to the August 24, 2016 Mw 6 Amatrice earthquake. We realized a three dimensional coseismic displacement field by combining different geodetic solutions generated by three independent analyses of the raw GPS observations. The coseismic deformation field described in this work aims at representing a consensus solution that minimizes the systematic biases potentially present in the individual geodetic solutions. Because of the limited number of stations available we modeled the measured coseismic displacements using a uniform slip model, deriving the geometry and kinematics of the causative fault, finding good agreement between our geodetically derived fault plane and other seismological and geological observations.?
机译:我们使用连续的全球定位系统(GPS)测量来推断与2016年8月24日Mw 6阿马特里奇地震相关的断层几何形状和同震滑动量。通过结合对原始GPS观测值的三个独立分析生成的不同大地测量解,我们实现了三维同震位移场。这项工作中描述的同震形变场旨在代表一种共识解决方案,该解决方案可以最大程度地减少各个大地测量解决方案中可能存在的系统偏差。由于可用站的数量有限,我们使用统一的滑动模型对测得的同震位移进行建模,推导了造成性断层的几何特征和运动学,在我们的大地测量断层平面与其他地震和地质观测结果之间找到了很好的一致性。

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