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Velocity Structure of the Subducted Yakutat Terrane, Alaska: Insights From Guided Waves

  • Published:2018-04-16 Issue:8 Volume:45 Page:3420-3428
  • ISSN:0094-8276
  • Container-title:Geophysical Research Letters
  • language:en
  • Short-container-title:Geophys. Res. Lett.

Author:

Coulson S.12ORCID,Garth T.13ORCID,Rietbrock A.14

Affiliation:

1. Department of Earth, Ocean and Ecological Sciences; University of Liverpool; Liverpool UK

2. Now at Department of Earth and Planetary Sciences; Harvard University; Cambridge MA USA

3. Now at Department of Earth Sciences; University of Oxford; Oxford UK

4. Now at Geophysical Institute; Karlsruhe Institute of Technology; Karlsruhe Germany

Funder

Harvard University

Frank Knox Memorial Fellowships

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference30 articles.

1. Hydrated subducted crust at 100-250 km depth;Abers;Earth and Planetary Science Letters,2000

2. Seismic low-velocity layer at the top of subducting slabs: Observations, predictions, and systematics;Abers;Physics of the Earth and Planetary Interiors,2005

3. Dispersion of regional body waves at 100-150 km depth beneath Alaska: In situ constraints on metamorphism of subducted crust;Abers;Geophysical Research Letters,1996

4. Alaska Earthquake Centre 2016 AEIC Earthquake Database

5. Parallel 3-D viscoelastic finite difference seismic modelling;Bohlen;Computers & Geosciences,2002

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