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Path-specific Velocity Structure of Western China from Surface-wave Dispersion

机译:从面波频散看中国西部路径特异速度结构

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We develop one-dimensional (1-D) path-specific velocity models in western China using new Rayleigh and Love wave group and phase velocity dispersion measurements for 20 events in the region. The earthquakes were grouped into three geographic clusters from which we compute the average phase and group velocity dispersion. We invert the average dispersion curves simultaneously for 1-D shear-velocity models appropriate for the three central Asian paths, using three previous shear-velocity models as initial models. The models are validated by forward modeling waveforms of recent events. The crustal thickness beneath western China in the vicinity of the Lop Nor test site is 50–60 km and our velocity models are consistent with major geologic features (e.g., basins and mountain ranges) and previous structural models for this region.
机译:我们使用新的瑞利波和洛夫波群以及该地区20个事件的相速度色散测量结果,开发了中国西部的一维(1-D)路径特定速度模型。地震被分为三个地理簇,据此我们可以计算平均相位和群速度散布。我们使用三个先前的剪切速度模型作为初始模型,同时反转了适合于三个中亚路径的一维剪切速度模型的平均频散曲线。通过最近事件的正向建模波形来验证模型。罗布泊试验场附近的中国西部地壳厚度为50-60 km,我们的速度模型与该地区的主要地质特征(如盆地和山脉)和以前的构造模型一致。

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