Beyond receiver functions: Passive source reverse time migration and inverse scattering of converted waves
We present a wave equation prestack depth migration to image crust and mantle structures using multi-component earthquake data recorded at dense seismograph arrays. Transmitted P and S waves recorded on the surface are back propagated using an elastic wave equation solver. The wave modes are separat...
Main Authors: | , , |
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Other Authors: | |
Format: | Article |
Language: | en_US |
Published: |
American Geophysical Union (AGU)
2012
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Online Access: | http://hdl.handle.net/1721.1/74214 https://orcid.org/0000-0003-1650-6818 |