Sediment Characterization at the Equatorial Mid‐Atlantic Ridge From P ‐to‐ S Teleseismic Phase Conversions Recorded on the PI‐LAB Experiment-Reference-Cited by-同舟云学术

Sediment Characterization at the Equatorial Mid‐Atlantic Ridge From P ‐to‐ S Teleseismic Phase Conversions Recorded on the PI‐LAB Experiment

Author:

Agius M. R.¹²^ORCID,Harmon N.¹^ORCID,Rychert C. A.¹^ORCID,Tharimena S.¹³^ORCID,Kendall J.‐M.⁴

Affiliation:

1. Ocean and Earth ScienceUniversity of Southampton Southampton UK

2. Now at the Department of GeosciencesFaculty of Science, University of Malta Msida Malta

3. Now at Jet Propulsion LaboratoryCalifornia Institute of Technology Pasadena CA USA

4. School of Earth SciencesUniversity of Bristol Bristol UK

Funder

Seventh Framework Programme

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

Reference37 articles.

1. Quantification of neogene and quaternary sediment input to the Madeira Abyssal Plain;Alibés B.;Geogaceta,1996

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