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By David E. Smith, Donald L. Turcotte

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Published by means of the yank Geophysical Union as a part of the Geodynamics Series.

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H. Jordan, P. Molnar, and E. Haines, Numerical deformationusing the global positioningsystem,Annu. Rev. Earth Planet. , 19, 351-382, 1991. J. R. , 36, 541-576, 1974. , and W. B. Myers, Cenozoictectonicsof the western UnitedStates,Rev. , 4, 509-549, 1966. , Continentaltectonicsin the aftermathof plate tectonics, Nature, 335, 131-137, 1988. , and I. S. Sacks,Subduction of the Nazeaplatebeneath Morgan, W. , Rises, trenches,great faults, and crustalblocks,J. GeoPem as determined from seismicobservations, J.

S. Stein, and A. Gripp, A modelfor the motionof the Phillipinc Sea Plateconsistent with NUVEL-1, J. Res, in press, 1993. somepredictions, J. , 77, 2087-2103, 1972. Sieh, K. , andT. H. , 17, 195-198, 1990. ,4, editedby D. W. SimpsonandP. G. Richards, Lawson,A. , The CaliforniaEarthquakeof April 18, 1906: pp. , 1981. Reportof the StateEarthquake Investigation Cornmission, Carnegie Sieh, K. , and R. , 1908. Wallace Creek, California, Geol. Soc. Am. , 95, 883-896, 1984. , Sea-floorspreading and continental drift,J.

Because of the larger velocity at Huahine, the plate. The lengths of the estimated residual vectors are relative rates from Huahine to Kwajelein and Kauai imply shorter than the modeled vector residual since a portion of some compression(Figure 12), but at a level just twice that the compressive strain is accommodatedbetween the sites of the standard deviation. and the subductionboundary. seen 34 at the Hawaiian ROBBINS ET AL. Conversely,the inclusionof VLBI and SLR information into solutions containing GPS information would provide an extra decadeof measurements spanningthe time when GPS was in its infancy.

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