- 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 sti...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Publisher's version
- Files:
-
-
(pdf, 2.9mb)
-
- Publisher copy:
- 10.1111/j.1365-246X.2012.05499.x
-
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- Publisher:
- Oxford University Press Publisher's website
- Journal:
- Geophysical Journal International Journal website
- Volume:
- 190
- Issue:
- 1
- Pages:
- 553-568
- Publication date:
- 2012-07-01
- DOI:
- EISSN:
-
1365-246X
- ISSN:
-
0956-540X
- URN:
-
uuid:9782eeda-0d91-4871-a5cd-b0ceab1f8a50
- Source identifiers:
-
582986
- Local pid:
- pubs:582986
- Copyright holder:
- Koelemeijer et al.
- Copyright date:
- 2012
- Notes:
- © 2012 The Authors. Geophysical Journal International © 2012 RAS.
Journal article
Normal mode sensitivity to Earth's D″ layer and topography on the core-mantle boundary: What we can and cannot see
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