Titlebook: Imaging the Rupture Processes of Earthquakes Using the Relative Back-Projection Method; Theory and Applicati Hao Zhang Book 2018 Springer-V

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https://doi.org/10.1007/978-3-662-55239-1Anti-earthquake Emergency Response; Beamforming; Generalized Array Imaging; Relative Back-Projection Me

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Back-Projection Imaging the 2010 Mw 8.8 Chilean Earthquake,On February 27, 2017, at 06:34:00 (UTC) an Mw 8.8 megathrust earthquake struck nearby Concepcion, South Chile, where the Nazca plate is subducting beneath the overriding South American plate. The earthquake was located at (35.905°S, 72.733°W) at a focal depth of 35 km (provided by USGS).

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Book 2018ow of a reference station; this led to a faster and more accurate image of the rupture processes of earthquakes. Mitigating the damage caused by earthquakes is one of the primary goals of seismology, and includes saving more people’s lives by devising seismological approaches to rapidly analyze an e

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Introduction,jection method, which can effectively and accurrately image the rupture processes of large earthquakes. This chapter briefly introduces the development of this technique and different flavors of the method. More importantly, the advantages and disadvantages of the method are elaborated.

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Generalized Array Imaging on Rupture Processes of Earthquakes: Principle and Theoretical Tests,e technique. To further validate the method, synthesized waveforms are generated to apply the back-projection the procedure. The resultant imaging supports the argument that the relative back-projection method can mitigate the “swimming” artifacts in the traditional back-projection imaging results.

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Imaging the 2008 Mw 7.8 Wenchuan Earthquake Using the Relative Back-Projection Method, damage as well as loss of human lives. Rapid estimation of the rupture process is essential for emergency response. In this paper, the relative back-projection method based on non-plane-wave array technology was applied to reconstruct the rupture process of this earthquake. First, the principle of