CaltechAUTHORS
  A Caltech Library Service

P and S Wave Travel Time Inversions for Subducting Slab Under the Island Arcs of the Northwest Pacific

Zhou, Hua-Wei and Clayton, Robert W. (1990) P and S Wave Travel Time Inversions for Subducting Slab Under the Island Arcs of the Northwest Pacific. Journal of Geophysical Research B, 95 (B5). pp. 6829-6851. ISSN 0148-0227. http://resolver.caltech.edu/CaltechAUTHORS:20121015-111307619

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

1723Kb

Use this Persistent URL to link to this item: http://resolver.caltech.edu/CaltechAUTHORS:20121015-111307619

Abstract

We have observed slablike high P and S velocity anomalies around the Wadati-Benioff zone under island arcs of the northwest Pacific through travel time tomographic inversions. Nineteen years of International Seismological Centre travel time residuals for events and stations in this large region are used. Analyses of resolution and noise show that the images are generally well resolved. The images illustrate that slab anomalies are continuous along strike in most parts of the upper mantle of the region and become contorted and generally broadened with depth. Near the bottom of the upper mantle, fingering of the slabs, including segmenting and spreading, is indicated. The fast anomalies associated with the Japan, Izu-Bonin, and Mariana subduction zones tend to flatten to subhorizontal at depth, while downward spreading may occur under parts of the Mariana and Kurile arcs. The fast anomalies below 700 km are not in the shape of a single coherent sheet. The principal compressional axes of focal mechanisms in the region consistently follow the downdip direction of the high-velocity slab, even when it bends to subhorizontal at depth. The depth at which compression begins to dominate the downdip stress regime in the slab apparently depends on bending of the slab and its dip. Slab fingering and intense deep seismicity probably are the consequence of the slab encountering a barrier of some form around the “670-km” discontinuity.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1029/JB095iB05p06829DOIUNSPECIFIED
http://www.agu.org/pubs/crossref/1990/JB095iB05p06829.shtmlPublisherUNSPECIFIED
Additional Information:© 1990 American Geophysical Union. Received 26 September 1988; revised November 10, 1989; accepted 5 October 1989. We thank Don L. Anderson for stimulating discussions and critical reading of the manuscript. Some useful comments by T. Tanimoto are appreciated. Several thorough, anonymous reviews improved the text. Work was supported by National Science Foundation grants EAR 83-17623. Contribution No. 4627, Division of Geological and Planetary Sciences, California Institute of Technology.
Funders:
Funding AgencyGrant Number
NSFEAR 83-17623
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences4627
Record Number:CaltechAUTHORS:20121015-111307619
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20121015-111307619
Official Citation:Zhou, H.-W. and R. W. Clayton (1990), P and S wave travel time inversions for subducting slab under the island arcs of the northwest Pacific, J. Geophys. Res., 95(B5), 6829–6851, doi:10.1029/JB095iB05p06829.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:34894
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:15 Oct 2012 18:34
Last Modified:27 Dec 2012 02:52

Repository Staff Only: item control page