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GEOPHYSICAL RESEARCH LETTERS,
VOL. 31,
L15S15,
doi:10.1029/2003GL019378,
2004
Re-evaluation of heat flow data near Parkfield, CA: Evidence for a weak San Andreas Fault
Patrick M. Fulton
Department of Geology and Geophysics, University of Wyoming, USA
Demian M. Saffer
Department of Geology and Geophysics, University of Wyoming, USA
Robert N. Harris
Department of Geology and Geophysics, University of Utah, USA
Barbara A. Bekins
U.S. Geological Survey, Menlo Park, California, USA
Abstract
Improved interpretations of the strength of the San Andreas Fault near Parkfield, CA based on thermal data require quantification
of processes causing significant scatter and uncertainty in existing heat flow data. These effects include topographic refraction,
heat advection by topographically-driven groundwater flow, and uncertainty in thermal conductivity. Here, we re-evaluate the
heat flow data in this area by correcting for full 3-D terrain effects. We then investigate the potential role of groundwater
flow in redistributing fault-generated heat, using numerical models of coupled heat and fluid flow for a wide range of hydrologic
scenarios. We find that a large degree of the scatter in the data can be accounted for by 3-D terrain effects, and that for
plausible groundwater flow scenarios frictional heat generated along a strong fault is unlikely to be redistributed by topographically-driven
groundwater flow in a manner consistent with the 3-D corrected data.
Received 28
December
2003;
accepted 5
March
2004;
published 24
June
2004.
Index Terms: 8130 Tectonophysics: Heat generation and transport; 8150 Tectonophysics: Plate boundary—general (3040); 8164 Tectonophysics: Stresses—crust and lithosphere.
Read Full Article (file size: 510071 bytes) Cited by
Citation: Fulton, P. M., D. M. Saffer, R. N. Harris, and B. A. Bekins
(2004),
Re-evaluation of heat flow data near Parkfield, CA: Evidence for a weak San Andreas Fault,
Geophys. Res. Lett.,
31,
L15S15,
doi:10.1029/2003GL019378.
Copyright 2004 by the American Geophysical Union.
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