Insights into exhumation and mantle hydration processes at the Deep Galicia margin from a 3D high-resolution seismic velocity model-Reference-Cited by-同舟云学术

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Insights into exhumation and mantle hydration processes at the Deep Galicia margin from a 3D high-resolution seismic velocity model

Published:2022-07-15 Issue: Volume: Page:
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Author:

Boddupalli Bhargav¹^ORCID,Minshull Timothy A²^ORCID,Bayrakci Gaye³,Lymer Gael⁴^ORCID,Klaeschen Dirk⁵^ORCID,Reston Timothy J.⁶^ORCID

Affiliation:

1. University of Texas at Austin

2. University of Southampton

3. Unknown

4. University College Dublin

5. GEOMAR Helmholtz Centre for Ocean Research Kiel

6. University of Birmingham

Publisher

Wiley

Reference40 articles.

1. Bayrakci G. Minshull T. A. Boddupalli B. Davy R. G. Klaeschen D. Papenberg C. etal (2022). Ocean bottom seismic data from the continent-ocean transition in the Deep Galicia Margin offshore West Iberia. PANGAEA. https://doi.org/10.1594/PANGAEA.940656

2. Fault-controlled hydration of the upper mantle during continental rifting;Bayrakci G.;Nature Geoscience,2016

3. Comparison of two- and three-dimensional full waveform inversion imaging using wide-angle seismic data from the Deep Galicia Margin;Boddupalli B.;Geophysical Journal International,2021

4. Undercrusting by serpentinite beneath rifted margins;Boillot G.;Nature,1989

5. Ocean-continent boundary of the Iberian margin: A serpentinite diapir west of the Galicia Bank;Boillot G.;Earth and Planetary Science Letters,1980

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