Reverse-time migration-based reflection tomography using teleseismic free surface multiples

Converted and multiply reflected phases from teleseismic events are routinely used to create structural images of the crust–mantle boundary (Moho) and the elasticity contrasts within the crust and upper mantle. The accuracy of these images is to a large extent determined by the background velocity m...

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Bibliographic Details
Main Authors: Burdick, S., de Hoop, Maarten, Wang, S., van der Hilst, Robert D
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: Oxford University Press on behalf of The Royal Astronomical Society 2014
Online Access:http://hdl.handle.net/1721.1/90857
https://orcid.org/0000-0003-1650-6818