Hydrothermal Models Constrained by Fine‐Scale Seismic Velocities Confirm Hydrothermal Cooling of 7–63 Ma South Atlantic Crust

Author:

Kardell Dominik A.12ORCID,Zhao Zeyu1,Ramos Evan J.3ORCID,Estep Justin4ORCID,Christeson Gail L.1ORCID,Reece Robert S.5ORCID,Hesse Marc A.36ORCID

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 Spring 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

6. Oden Institute for Computational Science and Engineering The University of Texas at Austin Austin TX USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference91 articles.

1. Hydrothermal alteration of a 1 km section through the upper oceanic crust, Deep Sea Drilling Project Hole 504B: Mineralogy, chemistry and evolution of seawater-basalt interactions

2. The role of outcrop‐to‐outcrop fluid flow in off‐axis oceanic hydrothermal systems under abyssal sedimentation conditions;Anderson B. W.;Journal of Geophysical Research,2012

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

4. Seismic Structure of the Upper Crust From 0–75 Ma in the Equatorial Atlantic Ocean on the African Plate Using Ultralong Offset Seismic Data

5. Inferring crustal structure in the Aleutian island arc from a sparse wide‐angle seismic data set;Avendonk H. J. A.;Geochemistry, Geophysics, Geosystems,2004

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