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...

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Bibliographic Details
Main Authors: Shang, Xuefeng, Hoop, Maarten V. de, van der Hilst, Robert D
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: American Geophysical Union (AGU) 2012
Online Access:http://hdl.handle.net/1721.1/74214
https://orcid.org/0000-0003-1650-6818