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A complex network model for seismicity based on mutual information

机译:基于互信息的地震活动复杂网络模型

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Seismicity is the product of the interaction between the different parts of the lithosphere. Here, we model each part of the Earth as a cell that is constantly communicating its state to its environment. As a neuron is stimulated and produces an output, the different parts of the lithosphere are constantly stimulated by both other cells and the ductile part of the lithosphere, and produce an output in the form of a stress transfer or an earthquake. This output depends on the properties of each part of the Earth's crust and the magnitude of the inputs. In this study, we propose an approach to the quantification of this communication, with the aid of the Information Theory, and model seismicity as a Complex Network. We have used data from California, and this new approach gives a better understanding of the processes involved in the formation of seismic patterns in that region.
机译:地震活动是岩石圈不同部分之间相互作用的产物。在这里,我们将地球的每个部分建模为一个不断向环境传达其状态的单元。当神经元受到刺激并产生输出时,岩石圈的不同部分会同时受到其他细胞和岩石圈的延性部分的刺激,并以应力传递或地震的形式产生输出。该输出取决于地壳各部分的性质以及输入的大小。在这项研究中,我们提出了一种利用信息论对这种通信进行量化的方法,并将地震活动性建模为一个复杂网络。我们使用了来自加利福尼亚的数据,这种新方法可以更好地理解该地区地震波型形成过程。

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