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Award Abstract #0216626
Leveraged acquisition of a Seattle fault GPS network: Four dimensional constraint on seismic and aseismic strain accumlation and release in the urbanized Puget Lowlands


NSF Org: EAR
Division of Earth Sciences
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Initial Amendment Date: July 29, 2002
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Latest Amendment Date: July 29, 2002
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Award Number: 0216626
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Award Instrument: Standard Grant
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Program Manager: Russell C. Kelz
EAR Division of Earth Sciences
GEO Directorate for Geosciences
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Start Date: August 1, 2002
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Expires: July 31, 2006 (Estimated)
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Awarded Amount to Date: $225000
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Investigator(s): M. Meghan Miller meghan@cwu.edu (Principal Investigator)
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Sponsor: Central Washington University
400 E. University Way
Ellensburg, WA 98926 509/963-2111
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NSF Program(s): MAJOR RESEARCH INSTRUMENTATION
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Field Application(s): 0000099 Other Applications NEC
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Program Reference Code(s): OTHR, 1189, 0000
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Program Element Code(s): 1189

ABSTRACT

0216626

Miller

Continuous observations using Global Positioning System (GPS) geodesy yield high-precision determination of horizontal and vertical deformation rates and their variation in time and space. This project builds on the stunning advances that data from the regional Pacific Northwest Geodetic Array (PANGA) has yielded over the last year. In partnership with the surveying community in Puget Sound, PANGA scientists will install a continuous GPS network that is optimally designed to determine the kinematics and locking of the Seattle fault zone, a major fault within the North America plate. In addition, this network provides important new constraints on the periodic recurrence of slow or silent earthquakes, which have been recently discovered along the transition zone of the Cascadia plate interface. Both studies have fundamental importance to characterizing the geodynamics of plate interaction, they also have broader impacts on quantifying seismic strain energy accumulation on a crustal fault that lies in the heart of the urbanized Puget Lowlands. This network will add new constraints to the relative balance between seismic and aseismic strain release mechanisms on the plate boundary fault that is known to generate great earthquakes (approximately magnitude 9) at frequencies of about 500 years. Finally, this project will foster the nascent collaboration between regional professional and academic communities.

The Puget Sound surveying community has formed a consortium to support coordination of new GPS technology to the urbanized Puget Lowlands. This collaboration of cities, counties, state agencies, and engineering firms is committed to installing a "virtual reference system" GPS network known as the Puget Reference System Utility (PRSU) that can provide cm-level positioning in real time. Fortuitously, this network is optimal for the earthquake and geodynamics studies outlined above, with the caveat that the solid earth deformation community has the highest standards for monumentation in order that GPS antennas track real earth motion rather than the effects of soil, gourndwater or man-made structures. The Puget Lowlands present the greatest first-order challenges to stable monument design: thick soil horizons, deep sedimentary basins in the foot wall of the Seattle fault and a mantle of debris left behind in the last glacial retreat require use of the deeply anchored drilled braced monument. Such monumentation is thus critical to making geophysically meaningful observations of great precision required by the problems posed here. This project funds geodetic quality monuments in order to leverage the PRSU GPS network for solid earth deformation studies in a highly leveraged fashion.

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PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

(Showing: 1 - 2 of 2).

A. M. Miner, M. M. Miller, and V. M., Santillan.  "Progress towards a multiple-use GPS array in the Puget Sound region,"  Eos, Transactions, American Geophysical Union,  v.85,  2004, 

M. E. Caron, M. M. Miller, and D. J. Johnson.  "Neotectonic crustal deformation and seismic hazard in the Puget Sound area of the Casdacia fore-arc, Washington State,"  Eos, Transactions, American Geophysical Union,  v.83,  2002, 


(Showing: 1 - 2 of 2).

 

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Last Updated:April 2, 2007