Global isostatic geoid anomalies for plate and boundary layer models of the lithosphere
Isostatic geoid anomalies are usually interpreted using a flat-earth, one-dimensional idealization. Isostatic anomalies on the spherical, self-gravitating earth differ from this idealization because: (1) degree one terms in the spherical harmonic expansion vanish; (2) each term in the spherical harm...
| Published in: | Earth and Planetary Science Letters |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
Elsevier
1983
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| Subjects: | |
| Online Access: | https://doi.org/10.1016/0012-821X(83)90025-0 |