Investigating Fine‐Scale Permeability Structure and Its Control on Hydrothermal Activity Along a Fast‐Spreading Ridge (the East Pacific Rise, 9°43′–53′N) Using Seismic Velocity, Poroelastic Response, and Numerical Modeling-Reference-Cited by-同舟云学术

Investigating Fine‐Scale Permeability Structure and Its Control on Hydrothermal Activity Along a Fast‐Spreading Ridge (the East Pacific Rise, 9°43′–53′N) Using Seismic Velocity, Poroelastic Response, and Numerical Modeling

Published:2019-11-05 Issue:21 Volume:46 Page:11799-11810
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Marjanović Milena¹^ORCID,Barreyre Thibaut²^ORCID,Fontaine Fabrice J.¹³,Escartín Javier¹^ORCID

Affiliation:

1. Université de Paris, Institut de Physique du Globe de Paris, CNRS Paris France

2. Department of Earth Science/K. G. Jebsen Centre for Deep Sea Research University of Bergen Bergen Norway

3. Now at Observatoire du Piton de la Fournaise Ile de La Réunion France

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084040

Reference85 articles.

1. Seismic evidence that black smoker heat flux is influenced by localized magma replenishment and associated increases in crustal permeability

2. Structure, Seismicity, and Accretionary Processes at the Hot Spot‐Influenced Axial Seamount on the Juan de Fuca Ridge

3. Fine-scale velocity structure of upper oceanic crust from full waveform inversion of downward continued seismic reflection data at the Lucky Strike Volcano, Mid-Atlantic Ridge

4. Nature of upper crust beneath the Lucky Strike volcano using elastic full waveform inversion of streamer data

5. Strong seismic heterogeneity in layer 2A near hydrothermal vents at the Mid-Atlantic Ridge

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