Tectonic Activity Near the Rio Grande Rise Increases Fluid Flux in Old Oceanic Crust-Reference-Cited by-同舟云学术

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Tectonic Activity Near the Rio Grande Rise Increases Fluid Flux in Old Oceanic Crust

Published:2021-09-02 Issue:17 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

Kardell Dominik A.¹²^ORCID,Zhao Zeyu¹,Ramos Evan J.³^ORCID,Estep Justin⁴^ORCID,Christeson Gail L.¹^ORCID,Reece Robert S.⁵^ORCID

Affiliation:

1. Jackson School of Geosciences Institute for Geophysics The University of Texas at Austin Austin TX USA

2. Now at ExxonMobil Upstream Integrated Solutions Houston TX USA

3. Department of Geological Sciences Jackson School of Geosciences The University of Texas at Austin Austin TX USA

4. School of Earth and Sustainability Northern Arizona University Flagstaff AZ USA

5. Department of Geology and Geophysics Texas A&M University College Station TX USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL094624

Reference51 articles.

1. Oceanic faulting and fault-controlled subseafloor hydrothermal alteration in the sheeted dike complex of the Josephine Ophiolite

2. Depth-Dependent Permeability and Heat Output at Basalt-Hosted Hydrothermal Systems Across Mid-Ocean Ridge Spreading Rates

3. Poroelastic response of mid‐ocean ridge hydrothermal systems to ocean tidal loading: Implications for shallow permeability structure

4. Modes of faulting at mid-ocean ridges

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