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• W1520540070 endingPage "207" @default.
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• W1520540070 abstract "The 1969–1984 history of seismic slip on the Calaveras fault in central California can be used to examine how slip is distributed in time and is partitioned between different deformation processes. Nowhere is there evidence that brittle deformation is the predominant failure mode over the entire depth range for which small earthquakes can be located (between about 2 and 15 km). The closest approach to completely brittle strain release occurs only for a more limited range of depths in a part of the region that ruptured during the 1984 Morgan Hill earthquake. Elsewhere aseismic deformation appears to contribute substantially to the total deformation. Except for the Hollister Valley, it is not known whether creep occurs on the fault, or in the surrounding media. In the Hollister Valley, creepmeter data suggest that fault creep can entirely accommodate the slip. Previous work indicates that rupture on the Calaveras fault, in both the Coyote Lake and Morgan Hill earthquakes, initiated and terminated at bends or offsets. Mechanisms invoking purely brittle and elastic behavior have been offered to explain observations of this type. The results that we present suggest that creep, as well as elastic-brittle processes, must play an important role in the micro-mechanics of these regions." @default.
• W1520540070 created "2016-06-24" @default.
• W1520540070 creator A5024637858 @default.
• W1520540070 creator A5052606209 @default.
• W1520540070 creator A5056027481 @default.
• W1520540070 date "2013-03-18" @default.
• W1520540070 modified "2023-10-17" @default.
• W1520540070 title "Seismic Slip, Aseismic Slip, and the Mechanics of Repeating Earthquakes on the Calaveras Fault, California" @default.
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• W1520540070 doi "https://doi.org/10.1029/gm037p0195" @default.
• W1520540070 hasPublicationYear "2013" @default.
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