CaltechAUTHORS
  A Caltech Library Service

Global Mapping of the Uppermantle by Surface Wave Tomography

Anderson, Don L. (1987) Global Mapping of the Uppermantle by Surface Wave Tomography. In: Composition, structure, and dynamics of the lithosphere-asthenosphere system. Geodynamics series. No.16. American Geophysical Union , Washington, DC, pp. 89-97. ISBN 9780875905181. https://resolver.caltech.edu/CaltechAUTHORS:20140508-125605076

[img]
Preview
PDF - Published Version
See Usage Policy.

660kB

Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20140508-125605076

Abstract

Surface wave tomography compliments detailed body wave studies by providing a global framework for the lateral variability of the uppermantle. In particular the method allows one to map the mantle beneath the lithosphere and to discuss the fate of overridden oceanic plates. Midocean ridges appear to extend to at least 400 km. By contrast, the very high velocities associated with shields are primarily much shallower. The Red Sea-Afar region is a pronounced and deep low-velocity anomaly. A significant uppermantle anomaly has been found in the central Pacific. This "Polynesian Anomaly" is surrounded by hotspots; Hawaii, Tahiti, Samoa and the Caroline Islands. This may be the site of the extensive Cretaceous volanism which generated the plateaus and seamounts in the western Pacific. Anisotropy indicates deep upwellings, >300 km depth, under midocean ridges, the Afar and the Polynesian Anomaly and downwelling under the western Pacific and the northeastern Indian Ocean. The large fast anomaly under the south Atlantic may represent overridden Pacific plate.


Item Type:Book Section
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1029/GD016p0089DOIArticle
http://onlinelibrary.wiley.com/doi/10.1029/GD016p0089/summaryPublisherArticle
Additional Information:© 1987 by the American Geophysical Union. I gratefully acknowledge the work of my colleagues Ichiro Nakanishi, Henri-Claude Nataf and Toshiro Tanimoto which forms the basis of the present paper. The figures were prepared by C. Stork. This research was supported by the National Science Foundation EAR-8115236 and EAR-8317623, and the National Aeronautics and Space Administration NSG-7610. Division of Geological and Planetary Sciences of the California Institute of Technology contribution number 4189.
Funders:
Funding AgencyGrant Number
NSFEAR-8115236
NSFEAR-8317623
NASANSG-7610
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences4189
Series Name:Geodynamics series
Issue or Number:16
DOI:10.1029/GD016p0089
Record Number:CaltechAUTHORS:20140508-125605076
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140508-125605076
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:45608
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:08 May 2014 21:15
Last Modified:10 Nov 2021 17:14

Repository Staff Only: item control page