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2D non-linear seismic response of the Dinar basin,TURKEY

机译:土耳其第纳尔盆地的二维非线性地震响应

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Local geological conditions generate significant amplification of ground motion and concentrated damage during earthquakes. The highly concentrated damages at the edges of the Dinar basin during occurred earthquakes at regions close to rock outcrop bring up the effect of the inclined bedrock effect on the dynamic behavior of the basin with 2D geometry. In this study, first the idealized 2D model of the basin based on the results of the underground explorations and geologic investigations is proposed. Results show that Dinar basin has an asymmetric 2D geometry with two different bedrock angles at edges. Then, a numerical study using finite difference based nonlinear code which utilizes appropriate static and dynamic boundary conditions, and includes hysteresis damping formulation based on the user defined degradation curves is conducted using real earthquake motions of different strength and frequency content. The constructed model is subjected to the collection of 16 earthquakes with different PGA's of 0.1, 0.2, 0.3 and 0.4 g, four motions for each PGA. It was seen that the dynamic behavior of the basin is broadly affected by the two dimensional bedrock. The results indicates the higher effect of the 6 degrees bedrock inclination at east part on the amplification with respect to the steeper 20 degrees bedrock slope at the west. Also, the results show the insignificant effect of the bedrock at the depth more than 150 m on the amplification of the east edge. While the effect of the 6 degrees bedrock angle at the east part continues until 1500 m from the outcrop, it affects the amplification until 700 m from the outcrop at the west part with 20 degrees bedrock angle. (C) 2016 Elsevier Ltd. All rights reserved.
机译:当地的地质条件在地震过程中会大大加剧地面运动并集中破坏。在靠近岩石露头的区域发生地震时,第纳尔盆地边缘的高度集中破坏引起了倾斜基岩效应对二维几何盆地动态行为的影响。在这项研究中,首先基于地下勘探和地质调查的结果提出了盆地的理想二维模型。结果表明,第纳尔盆地具有不对称的二维几何结构,边缘处具有两个不同的基岩角度。然后,使用具有不同强度和频率含量的真实地震运动,进行了基于有限差分的非线性代码的数值研究,该非线性代码利用了适当的静态和动态边界条件,并且包括了基于用户定义的退化曲线的磁滞阻尼公式。所构建的模型经受了16次地震的采集,这些地震具有0.1、0.2、0.3和0.4 g的不同PGA,每个PGA有四个运动。可以看出,该盆地的动态行为受到二维基岩的广泛影响。结果表明,相对于西部较陡的20度基岩坡度,东部6度基岩倾角对放大作用的影响更大。结果还表明,基岩在深度大于150 m时对东边缘的放大作用不明显。尽管东部的6度基岩角的影响一直持续到距露头1500 m,但它影响了放大作用,直到西部的20度基岩角距露头700 m。 (C)2016 Elsevier Ltd.保留所有权利。

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