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Volumn 282, Issue 5390, 1998, Pages 924-927

Seismic evidence for an inner core transition zone

Author keywords

[No Author keywords available]

Indexed keywords

DISCONTINUITY; INNER CORE; SEISMIC VELOCITY; TRANSITION ZONE; VELOCITY STRUCTURE;

EID: 0032582833     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.282.5390.924     Document Type: Article
Times cited : (136)

References (39)
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    • note
    • Unless otherwise noted, NS paths are used in this paper to mean those paths whose ray directions in the inner core are nearly parallel to (within 30°) Earth's spin axis, and EW paths are those whose ray directions in the inner core are nearly parallel (within 50°) to the equatorial plane.
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    • note
    • Supported by the National Science Foundation. This work would not be possible without open access to the IRIS Data Management Center and the German GEOFONE Data Center. We thank X. M. Ding, J. Cassidy, S. Malone, and R. Lester for assistance in data collection. Comments from two anonymous reviewers greatly improved the manuscript.


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