Strain accumulation along the San Andreas fault system east of San Francisco Bay, California
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Abstract
The occurrence of several large earthquakes to the east of San Francisco Bay during historical times, and present high levels of microseismicity, indicate that a significant part of the relative plate motion may be occurring east of San Francisco Bay. Furthermore, the Hayward fault is known to be slipping aseismically at the surface, and the Calaveras fault may be slipping aseismically also. These facts raise an important question: Is the observed creep rate accommodating all of the east bay deformation or is there a significant amount of strain accumulating along these faults?
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Strain accumulation along the San Andreas fault system east of San Francisco Bay, California |
| Series title | Tectonophysics |
| DOI | 10.1016/0040-1951(83)90124-5 |
| Volume | 97 |
| Issue | 1-4 |
| Year Published | 1983 |
| Language | English |
| Publisher | Elsevier |
| Description | 16 p. |
| First page | 41 |
| Last page | 56 |
| Country | United States |
| State | California |
| Other Geospatial | east of San Francisco Bay |