位置从一维反演地壳厚度估计表面波色散曲线——地球科学堆栈交换江南电子竞技平台江南体育网页版 最近30从www.hoelymoley.com 2023 - 07 - 09 - t00:45:00z //www.hoelymoley.com/feeds/question/284 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/284 22 放置1 d反转的地壳厚度估计表面波色散曲线 狮子座Uieda //www.hoelymoley.com/users/137 2014 - 04 - 17 - t14:49:04z 2015 - 03 - 20 - t17:12:03z < p >现在地震面波的色散行为特征不同频率不同的速度。这一特点< em > < / em >色散曲线取决于剪切和压缩波的地壳和上地幔速度结构。这些物理参数可以使用一些反演方法估计可以1 d, 2 d或3 d。一维反演相对简单和速度是非常普遍的。然而,分散两个站之间通常是测量<强> < / >强。< / p > < p >我的问题是,我们在哪里“地方”生成的1 d估计模型?站之间是地壳的平均水平(很久以前我做了数学这一次,似乎不是这样,但是我不确定)?还是没有办法估计在单点? < / p > //www.hoelymoley.com/questions/284/placement-of-crustal-thickness-estimation-from-1d-inversion-of-surface-wave-disp/290 # 290 12 Neo答案的位置从一维反演地壳厚度估计的表面波色散曲线 Neo //www.hoelymoley.com/users/32 2014 - 04 - 17 - t16:15:59z 2014 - 04 - 17 - t16:24:20z < p >这是一个很好的问题,对地震反演不仅重要,而且建模。< / p > < p >允许设置这个问题不同。假设A和D点的节点。< / p >

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Each node represents a system of equations, and these equations are only calculated on these points. Therefore, the model can only exist on the points in which they are calculated. Since B and C are dimensionally between A and D, a smoothing factor must be imposed to graphically represent them. So while there might be a line in between A and D, the model only exists on points A and D. To find the model at point B and C, you would have to build them in your model, creating a higher resolution mesh. This is perhaps why it is so important to have a dense seismic array when doing seismic studies.

So in your case, the model is dependent on information on information at two stations, making each node TWO STATIONS. This would mean that the it is impossible to give an exact geographic location to where the inversion is, just a generalized idea of between these two stations.

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