Published December 1983 | Version public
Journal Article

Solid earth geophysics

Abstract

Ten years ago seismologists were, or thought they were, putting the finishing touches on average Earth models, including the so-called radially symmetric reference Earth model, and were starting to devote their attention to lateral variations. It was clear, even then, that the mantle was heterogeneous everywhere, not just in the lithosphere and asthenosphere, but it was not clear how these anomalies related to surface tectonics.

Additional Information

© 1983 Geological Society of America.

Additional details

Identifiers

Eprint ID
45573
DOI
10.1130/0091-7613(1983)11<679:GAF>2.0.CO;2
Resolver ID
CaltechAUTHORS:20140507-115046107

Dates

Created
2014-05-07
Created from EPrint's datestamp field
Updated
2021-11-10
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Caltech Custom Metadata

Other Numbering System Name
Caltech Division of Geological and Planetary Sciences
Other Numbering System Identifier
3962