in collaboration with:
Steve Constable (IGPP), Antony White and Graham Heinson (Flinders University, Adelaide)
Goto:
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![]() The Moana Wave |
age groups: 4- 20 myrs 20- 52 myrs 52-110 myrs > 110 myrs(above, left hand side) Shear velocity models for oceanic lithosphere as a function of age (Nishimura and Forsyth, 1989). (right hand side) Group and phase velocities evaluated for the corresponding models on the left. Note that the line conventions in all 3 panels of this figure are the same.
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Resolution kernels obtained using the Backus-Gilbert method for various target depths (vertical bars). The 'data' used for the resolution test are phase velocities from 15-60s. The resolution kernels for depths > 80km vary significantly when data between 40-60s are omitted (not shown here). This indicates that data between 40-60s are necessary to resolve (sub-lithospheric) structure below 80km. Due to the increased long-period noise induced by ocean gravity waves, useful signal above 60s will only be obtained for the largest earthquakes (Ms > 7.0). |
Electrical model of generic plume and swell structure. Resistivity values are based on controlled source EM soundings, marine MT soundings, and laboratory studies of melt and subsolidus mantle rocks. | ![]() |
This project has been presented at the following meetings: |
IASPEI 29th General Assembly, August 18-28, 1997, Thessaloniki, Greece |
AGU Spring 98 meeting, May 26-29, 1998, Boston |
AGU Fall 98 meeting, December 6-10, 1998, San Francisco |
IUGG 22nd General Assembly, July 18-30, 1999, Birmingham, England |
AGU Fall 99 meeting, Dec 13-17, 1999, San Francisco |
SSA 95th Annual Meeting, Apr 10-12, 2000, San Diego |
12th Annual IRIS Workshop, May 09-11, 2000, Samoset Resort, Maine |
PLUME 3 Conference, Jun 18-24, 2000, Four Seasons Resort, Hawaii |
AGU Fall 2000 meeting, Dec 15-19, 2000, San Francisco |
This research is funded by the National Science Foundation.
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