Correction to “Slip rate of the Calico fault: Implications for geologic versus geodetic rate discrepancy in the Eastern California Shear Zone”

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منابع مشابه

Paleoseismology and Global Positioning System: Earthquake-cycle effects and geodetic versus geologic fault slip rates in the Eastern California shear zone

doi: 10.1130/0091-7613(2003)031<0055:PAGPSE>2.0.CO;2 2003;31;55-58 Geology Timothy H. Dixon, E. Norabuena and L. Hotaling geodetic versus geologic fault slip rates in the Eastern California shear zone Paleoseismology and Global Positioning System: Earthquake-cycle effects and Email alerting services cite this article to receive free e-mail alerts when new articles www.gsapubs.org/cgi/alerts cli...

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Holocene slip rates along the Owens Valley fault, California: Implications for the recent evolution of the Eastern California Shear Zone

One of the largest historical earthquakes in California occurred in 1872 along the Owens Valley fault located along the western margin of the Eastern California Shear Zone. New paleoseismic and optically stimulated luminescence data are the first to bracket the timing of the pre-1872 rupture to between 3.3 6 0.3 and 3.8 6 0.3 ka. These data yield an earthquake recurrence interval between 4100 a...

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Temporal variations in slip rate of the White Mountain Fault Zone, Eastern California

The evolution of fault slip through time may yield insight into the geodynamics of deforming lithosphere. Precise determination of temporal variations in fault slip is often hindered, however, by a dearth of markers of varying age from which to reconstruct fault slip. Here we determine slip rates across the White Mountain Fault Zone over the past ca. 0.8 Ma from displaced alluvial deposits pres...

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Holocene slip rate of the Wasatch fault zone, Utah, from geodetic data: Earthquake cycle effects

[1] GPS data define a broad zone of present day deformation in the eastern Basin and Range province, western US. Using finite element models with elastic upper crust over viscoelastic lower crust/upper mantle and incorporating earthquake cycle effects, we show that these data are consistent with a model whereby most contemporary fault slip is focused on the Wasatch fault zone. Modeled rates of ...

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Using IRSL to determine the slip rate of the Doruneh fault in Khalilabad

Introduction   The left lateral Doruneh Fault System (DFS), is one of the longest, and most prominent, strike-slip faults in Iran, extending from the eastern border of Iran to the central Dasht-e-Kavir with a curved geometry. DFS is the response of the convergence between the Arabian and Eurasian plates in the regional tectonic map. Regarding to scaling relationships this fault with length of ...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research

سال: 2007

ISSN: 0148-0227

DOI: 10.1029/2007jb005222