Physics of Geochemical Mechanics and Deep Neural Network Modeling with Diffusion Augmentation

Physics of Geochemical Mechanics and Deep Neural Network Modeling with Diffusion Augmentation
Author :
Publisher : Springer
Total Pages : 0
Release :
ISBN-10 : 9819793750
ISBN-13 : 9789819793754
Rating : 4/5 (754 Downloads)

Book Synopsis Physics of Geochemical Mechanics and Deep Neural Network Modeling with Diffusion Augmentation by : Mitsuhiro Toriumi

Download or read book Physics of Geochemical Mechanics and Deep Neural Network Modeling with Diffusion Augmentation written by Mitsuhiro Toriumi and published by Springer. This book was released on 2024-12-07 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: This book provides a new data augmentation method based on the local stochastic distribution patterns in natural time series data of global and regional seismicity rates and their correlated seismicity rates. The augmentation procedure is called the diffusion - denoising augmentation method from the local Gaussian distribution of segmented data of long time series. This method makes it possible to apply the deep machine learning necessary to neural network prediction of rare large earthquakes in the global and regional earth system. The book presents the physical background of the processes showing the development of characteristic features in the global and regional correlated seismicity dynamics, which are manifested by the successive time series of 1990-2023. Physical processes of the correlated global seismicity change and the earth's rotation, fluctuation of plate motion, and the earth's ellipsoid ratio (C20 of satellite gravity change) are proposed in this book. The equivalency between Gaussian seismicity network dynamics and the minimal nonlinear dynamics model of correlated seismicity rates is also provided. In addition, the book contains simulated models of the shear crack jog wave, precipitation of minerals in the jog, and jog accumulation inducing shear crack propagation which leads to earthquakes in the plate boundary rocks under permeable fluid flow.


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