Jerry L. Svarc
J.C. Savage
W.H. Prescott
Weijun Gan
2000
<p><span>The motion of a linear array of monuments extending across the Eastern California Shear Zone (ECSZ) has been measured from 1994 to 1999 with the Global Positioning System. The linear array is oriented N54°E, perpendicular to the tangent to the local small circle drawn about the Pacific-North America pole of rotation, and the observed motion across the ECSZ is approximated by differential rotation about that pole. The observations suggest uniform deformation within the ECSZ (strike N23°W) (26 nstrain yr</span><sup><span>−1</span></sup><span><sup> </sup>extension normal to the zone and 39 nstrain yr</span><sup><span>−1</span></sup><span> simple right-lateral shear across it) with no significant deformation in the two blocks (the Sierra Nevada mountains and southern Nevada) on either side. The deformation may be imposed by right-lateral slip at depth on the individual major fault systems within the zone if the slip rates are: Death Valley-Furnace Creek fault 3.2±0.9 mm yr</span><sup><span>−1</span></sup><span>, Hunter Mountain-Panamint Valley fault 3.3±1.6 mm yr</span><sup><span>−1</span></sup><span>, and Owens Valley fault 6.9±1.6 mm yr</span><sup><span>−1</span></sup><span>. However, this estimate of the slip rate on the Owens Valley fault is 3 times greater than the geologic estimate.</span></p>
application/pdf
10.1029/2000JB900105
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AGU Publications
Strain accumulation across the Eastern California Shear Zone at latitude 36°30'N
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