H.J.A. Van Avendonk
Seismic structure and segmentation of the axial valley of the Mid-Cayman Spreading Center
Van Avendonk, H.J.A.; Hayman, N.W.; Harding, J.L.; Grevemeyer, I.; Peirce, C.; Dannowski, A.
Authors
N.W. Hayman
J.L. Harding
I. Grevemeyer
Professor Christine Peirce christine.peirce@durham.ac.uk
Professor
A. Dannowski
Abstract
We report the results of a two-dimensional tomographic inversion of marine seismic refraction data from an array of ocean-bottom seismographs (OBSs), which produced an image of the crustal structure along the axial valley of the ultraslow-spreading Mid-Cayman Spreading Center (MCSC). The seismic velocity model shows variations in the thickness and properties of the young oceanic crust that are consistent with the existence of two magmatic-tectonic segments along the 110 km-long spreading center. Seismic wave speeds are consistent with exhumed mantle at the boundary between these two segments, but changes in the vertical gradient of seismic velocity suggest that volcanic crust occupies most of the axial valley seafloor along the seismic transect. The two spreading segments both have a low-velocity zone (LVZ) several kilometers beneath the seafloor, which may indicate the presence of shallow melt. However, the northern segment also has low seismic velocities (3 km/s) in a thick upper crustal layer (1.5-2.0 km), which we interpret as an extrusive volcanic section with high porosity and permeability. This segment hosts the Beebe vent field, the deepest known high-temperature black smoker hydrothermal vent system. In contrast, the southern spreading segment has seismic velocities as high as 4.0 km/s near the seafloor. We suggest that the porosity and permeability of the volcanic crust in the southern segment are much lower, thus limiting deep seawater penetration and hydrothermal recharge. This may explain why no hydrothermal vent system has been found in the southern half of the MCSC.
Citation
Van Avendonk, H., Hayman, N., Harding, J., Grevemeyer, I., Peirce, C., & Dannowski, A. (2017). Seismic structure and segmentation of the axial valley of the Mid-Cayman Spreading Center. Geochemistry, Geophysics, Geosystems, 18(6), 2149-2161. https://doi.org/10.1002/2017gc006873
Journal Article Type | Article |
---|---|
Acceptance Date | May 16, 2017 |
Online Publication Date | Jun 16, 2017 |
Publication Date | Jun 16, 2017 |
Deposit Date | Mar 6, 2017 |
Journal | Geochemistry, Geophysics, Geosystems |
Electronic ISSN | 1525-2027 |
Publisher | American Geophysical Union |
Peer Reviewed | Peer Reviewed |
Volume | 18 |
Issue | 6 |
Pages | 2149-2161 |
DOI | https://doi.org/10.1002/2017gc006873 |
Public URL | https://durham-repository.worktribe.com/output/1362193 |
You might also like
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2024
Advanced Search