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Three-dimensional structure of the Earth from splitting in free-oscillation spectra

Abstract:

Observations of splitting in free oscillations spectra can be used to constrain the three-dimensional distribution of heterogeneity in the Earth. Modes sampling mainly the Earth's mantle are compatible with the distributions of mantle heterogeneity inferred from P-wave travel times. The anomalously large splitting of modes penetrating deeply into the core requires large departures from sphericity which are difficult to accommodate within the framework of an isotropic model', it is argued that...

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Journal:
Nature
Volume:
325
Issue:
6103
Pages:
405-411
Publication date:
1987-01-01
ISSN:
0028-0836
Language:
English
Pubs id:
pubs:187605
UUID:
uuid:3e32cace-c7d0-4382-832b-61c5189e34bf
Local pid:
pubs:187605
Source identifiers:
187605
Deposit date:
2012-12-19

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