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MODELISATION OF TOPOGRAPHIC SITE EFFECT 3D AT THE LOW NOISE UNDERGROUND LABORATORY (LSBB), RUSTREL, FRANCE

机译:在法国RUSTREL的低噪声地下实验室(LSBB)进行的地形现场效果3D的修改

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The local geology related to topographic site effects is known to have a strong impact on the amplifications and attenuations of the ground motion. The SHAKE3D finite difference code [Cruz-Atienza et al., 2007] allows studying the influence of various local structures and rheological parameters on the seismic response at the surface. The ground motion is simulated in a realistic heterogeneous 3D model. This model integrates the mountainous topography above the Low Noise Underground Laboratory, Rustrel, France (http://lsbb.unice.fr)and the medium properties deduced from seismic imaging experiment done in 2006.Such a topography is typical in the South-East region of France : steep slope (greater than 30%) and sharp crest followed by a broad plateau. This configuration also allows investigation of coupled basin-topographic responses at the regional scale.We consider several models taking into account the spatial variation of the rheological parameters VP, VS, QP,QS, and density together with the topography. Sources with different locations and radiation patterns are also considered relatively to the geometry of the topography. These simulations help us to improve our knowledge of the topographic effects taking into account the heterogeneity of medium and the complexity of the topography.
机译:已知与地形现场影响有关的当地地质对地面运动的放大和衰减有很大的影响。 SHAKE3D有限差分代码[Cruz-Atienza et al。,2007]允许研究各种局部结构和流变参数对地表地震响应的影响。在逼真的异构3D模型中模拟了地面运动。该模型整合了法国Rustrel低噪声地下实验室上方的山区地形(http://lsbb.unice.fr)和2006年进行的地震成像实验得出的中等性质。法国地区:陡峭的坡度(大于30%)和陡峭的山顶,然后是宽阔的高原。这种配置还允许在区域尺度上研究盆地-地形耦合响应。我们考虑了几个模型,其中考虑了流变参数VP,VS,QP,QS和密度以及地形的空间变化。相对于地形的几何形状,还考虑了具有不同位置和辐射方向图的源。这些模拟考虑到介质的异质性和地形的复杂性,有助于我们提高对地形影响的认识。

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