- Abstract:
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We present seismic observations of the uppermost layer of the inner core. This was formed most recently, thus its seismic features are related to current solidification processes. Previous studies have only constrained the east-west hemispherical seismic velocity structure in the Earth’s inner core at depths greater than 15 km below the inner core boundary. The properties of shallower structure have not yet been determined, because the seismic waves PKIKP and PKiKP used for differential trave...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted Manuscript
- Files:
-
-
(pdf, 3.1mb)
-
- Publisher copy:
- 10.1016/j.pepi.2017.11.010
-
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- Funding agency for:
- Deuss, A
- Publisher:
- Elsevier Publisher's website
- Journal:
- Physics of the Earth and Planetary Interiors Journal website
- Volume:
- 274
- Pages:
- 158-169
- Publication date:
- 2017-11-28
- Acceptance date:
- 2017-11-27
- DOI:
- ISSN:
-
0031-9201
- Pubs id:
-
pubs:811317
- URN:
-
uri:045ea855-5fcc-42d1-b212-a6d86f92bc71
- UUID:
-
uuid:045ea855-5fcc-42d1-b212-a6d86f92bc71
- Local pid:
- pubs:811317
- Copyright holder:
- Elsevier B.V.
- Copyright date:
- 2017
- Notes:
- © 2017 Elsevier B.V. All rights reserved. This is the author accepted manuscript following peer review version of the article. The final version is available online from Elsevier at: 10.1016/j.pepi.2017.11.010
Journal article
Measuring the seismic velocity in the top 15 km of Earth’s inner core
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