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Normal mode sensitivity to Earth's D″ layer and topography on the core-mantle boundary: What we can and cannot see

Abstract:
The core-mantle boundary (CMB) is Earth's most profound internal boundary separating the liquid iron outer core and the solid silicate mantle. The detailed structure near the CMB has a major influence on mantle convection and the evolution of the core. Seismic observations, such as topography on the CMB, thin ultra-low velocity zones (ULVZs), seismic anisotropy and the anticorrelation between shear wave and bulk sound velocity heterogeneities have mainly been made using body waves and are still poorly constrained. We investigate the sensitivity of Earth's free oscillations to these features and specifically show how large individual anomalies must be for them to be observable. In addition, we discuss the possible trade-offs between these different lowermost mantle structures. Although modes have strong sensitivity to all the structures inserted, the results illustrate the limits of what normal modes can resolve. Our tests show that: (i) Even small scale features, such as ULVZs, with a thickness larger than 19km can be observed as long as their distribution contains a long wavelength component. (ii) The peak-to-peak amplitude of CMB topography has a larger influence than its pattern and has to be smaller than 5km to fit the data. (iii) The effect of scaling between shear wave velocity and density anomalies is less constrained, but a laterally varying pattern is implied by a simple test, suggesting the presence of chemical variations. (iv) A strong trade-off exists between anisotropy in compressional wave velocity and incidence angle whereas shear wave anisotropy is less observable. These findings provide valuable information for future normal mode studies on structures in Earth's lowermost mantle and their trade-offs.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1111/j.1365-246X.2012.05499.x

Authors

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author


More from this funder
Funding agency for:
Deuss, A
Grant:
Philip Leverhulme Prize
More from this funder
Funding agency for:
Koelemeijer, P
Grant:
Nahum Scholarship in Physics
Graduate Studentship
More from this funder
Funding agency for:
Koelemeijer, P
Deuss, A
Grant:
Graduate Studentship
Nahum Scholarship in Physics
Philip Leverhulme Prize


Publisher:
Oxford University Press
Journal:
Geophysical Journal International More from this journal
Volume:
190
Issue:
1
Pages:
553-568
Publication date:
2012-07-01
Acceptance date:
2012-04-15
DOI:
EISSN:
1365-246X
ISSN:
0956-540X


Keywords:
Pubs id:
pubs:582986
UUID:
uuid:9782eeda-0d91-4871-a5cd-b0ceab1f8a50
Local pid:
pubs:582986
Source identifiers:
582986
Deposit date:
2016-03-31
ARK identifier:

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