Velocity and anisotropy structure of the Icelandic crust - An ambient seismic noise analysis ...
Measuring the travel times of seismic waves is one of the most important tools for uncovering Earth’s structure and dynamics. In recent years, the discovery that surface wave dispersion could be estimated from ambient noise has introduced new possibilities into the field of seismic imaging, such as...
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| Format: | Thesis |
| Language: | English |
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Apollo - University of Cambridge Repository
2020
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| Online Access: | https://dx.doi.org/10.17863/cam.69617 https://www.repository.cam.ac.uk/handle/1810/322158 |
| Summary: | Measuring the travel times of seismic waves is one of the most important tools for uncovering Earth’s structure and dynamics. In recent years, the discovery that surface wave dispersion could be estimated from ambient noise has introduced new possibilities into the field of seismic imaging, such as performing passive source tomography in regions where it was not previously possible with a dense azimuthal ray path coverage. In this work, I leverage the new possibilities introduced by this method to investigate the crust in Iceland in a number of ways, including tomographic imaging as well as azimuthal and radial anisotropy analyses in both the lower and upper crust. Understanding accretion and deformation processes at mid-ocean ridges is crucial because they control the resulting oceanic crustal structure, which covers two-thirds of the Earth’s surface. Iceland, which is uplifted by a convective mantle plume and has an active spreading ridge system exposed above sea level, offers a unique opportunity for ... |
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