Isotropy overlying anisotropy at the top of the inner core

Geophysical Research Letters

Volumn 28, Issue 22, 2001, Pages 4331-4334

  Ouzounis, Aristeidis ^a   Creagar, Kenneth C ^a  

^a UNIVERSITY OF WASHINGTON   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

GEOLOGIC MODELS; GEOPHYSICS; STRUCTURAL GEOLOGY; EARTH SCIENCES;

ISOTROPY;

ANISOTROPY;

ANISOTROPY; INNER CORE; ISOTROPY; TRAVEL TIME;

INNER CORE; LARGE DATASET; LAYERED MODEL; LAYERED STRUCTURES; POSSIBLE MECHANISMS; STRONG ANISOTROPY; TRANSITION ZONES; TRAVEL-TIME RESIDUALS;

EID: 0035891816     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2001GL013341     Document Type: Article

References (19)

1. Inner core attenuation from short-period PKP (BC) versus PKP (DF) waveforms
2. Seismic attenuation of the inner core: Viscoelastic or stratigraphic?
3. Anisotropy of the inner core from differential travel times of the phases PKP and PKIKP
4. Inner core rotation rates from small-scale heterogeneity and time-varying travel times
5. Inner core anisotropy and rotation
6. Mapping heterogeneity of the uppermost inner core using two pairs of core phases
7. Constraints on seismic velocities in the Earth from travel times
8. Anisotropy of the inner core inferred from PKIKP travel times
9. Hemispherical variations in seismic velocity at the top of the Earth's inner core
10. Constraints on inner core anisotropy from ISC PKP(DF) travel times
11. Anisotropy of Earth's inner core
12. Depth dependence of anisotropy of Earth's inner core
13. Seismological evidence for differential rotation of Earth's inner core
14. Anisotropy of the Earth's inner core
15. Seismic evidence for an inner core transition zone
16. Joint inversion for inner core rotation, inner core anisotropy, and mantle heterogeneity
17. Limits of lateral density and velocity variations in the Earth's outer core
18. Degree one heterogeneity and hemispherical variation of anisotropy in the inner core from PKP(BC) - PKP(DF) times
19. Fine-scale heterogeneity in the Earth's Inner Core