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A feature of these methods is that the retrieved signals are naturally decomposed into up- and down-going components. Unlike 2Dmore » surveys, where profile positioning is flexible, 3 D surveys involve high density coverage over many square miles operated by numerous personnel. For this we used a regional 3 – D velocity model, recently obtained from full waveform inversion.

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Comparison with a similar dataset and subsequent 3 D velocity model acquired at the boundary between the and earthquakes will provide important insights into the segmentation of the Sumatra subduction zone and the dynamics of its great earthquakes. We divide our data into different epochs and invert two epochs simultaneously. The predictable. Heterogeneous characteristics of the Stracciacappa maar stratification, structural setting, lithotypes, and thickness variation of depositional units make it an ideal case history for understanding mechanisms and processes leading to modifications of amplitude-frequency-duration of seismic waves generated at earthquake sources and propagating through volcanic settings. In each of our

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