Heterogeneous upper mantle structure beneath the Ross Sea Embayment and Marie Byrd Land, West Antarctica, revealed by P-wave tomography
We present an upper mantle P-wave velocity model for the Ross Sea Embayment (RSE) region of West Antarctica, constructed by inverting relative P-wave travel-times from 1881 teleseismic earthquakes recorded by two temporary broadband seismograph deployments on the Ross Ice Shelf, as well as by region...
Main Authors: | , , , , , , , , , , , , |
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Format: | Text |
Language: | unknown |
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ScholarWorks@CWU
2019
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Subjects: | |
Online Access: | https://digitalcommons.cwu.edu/cotsfac/295 https://par.nsf.gov/biblio/10095101 |