Resolving the fine-scale velocity structure of continental hyperextension at the Deep Galicia Margin using full-waveform inversion-Reference-Cited by-同舟云学术

Resolving the fine-scale velocity structure of continental hyperextension at the Deep Galicia Margin using full-waveform inversion

Published:2017-10-03 Issue:1 Volume:212 Page:244-263
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Davy R G¹²,Morgan J V²,Minshull T A¹,Bayrakci G¹,Bull J M¹,Klaeschen D³,Reston T J⁴,Sawyer D S⁵,Lymer G⁴,Cresswell D⁴

Affiliation:

1. Ocean and Earth Science, University of Southampton, Southampton SO17 1BJ, United Kingdom

2. Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, United Kingdom. E-mail: r.davy@imperial.ac.uk

3. GEOMAR Helmholtz Centre for Ocean Research, D-24148 Kiel, Germany

4. University of Birmingham, Birmingham B15 2TT, United Kingdom

5. RICE University, Houston, TX 77005, USA

Funder

UK Natural Environment Research Council

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/212/1/244/27761116/ggx415.pdf

Reference50 articles.

1. Seismic evidence that black smoker heat flux is influenced by localized magma replenishment and associated increases in crustal permeability;Arnoux;Geophys. Res. Lett.,2017

2. Fault-controlled hydration of the upper mantle during continental rifting;Bayrakci;Nat. Geosci.,2016

3. Ocean-continent boundary in the Iberia Abyssal Plain from multichannel seismic data;Beslier;Tectonophysics,1993

4. Introduction, objectives, and principal results: Ocean Drilling Program Leg 103, west Galicia Margin;Boillot;Proc. Ocean Drill. Program, Initial Reports,1987

5. Three-dimensional geometries of rifting on a hyperextended margin-Interpretation of seismic reflection profiles from the Deep Galicia Basin, Iberia;Borgmeyer,2010

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