GPS-derived strain in northwestern California: Termination of the San Andreas fault system and convergence of the Sierra Nevada–Great Valley block contribute to southern Cascadia forearc contraction

Author:

Williams Todd B.,Kelsey Harvey M.,Freymueller Jeffrey T.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference39 articles.

1. The 1997 International Terrestrial Reference Frame (ITRF97);Boucher,1999

2. Seismotectonics of the San Andreas fault system between point arena and Cape Mendocino in Northern California: implication for the development and evolution of a young transform;Castillo;Journal of Geophysical Research,1993

3. Late Holocene tectonics and paleoseismicity, southern Cascadia subduction zone;Clarke;Science,1992

4. Kinematic models for Pacific–North America motion from 3 Ma to present: I. Evidence for steady state motion and biases in the NUVEL-1A model;DeMets;Geophysical Research Letters,1999

5. The September 1, 1994 Mendocino fault earthquake;Dengler;California Geology,1995

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