Abstract
Abstract On September 12, 1966, at 16h 41m, an earthquake of magnitude 6.0 to 6.5 occurred about 10 km northeast of Truckee, California. Hypocenters of 158 after-shocks that occurred between September 14 and 25 were found to be within a volume 3 km wide by 10 km long by 12 km deep. The magnitude-frequency curve appears anomalous, as there seem to be too many shocks greater than magnitude 2 compared to the number of small ones under magnitude 0.5. Nodal-plane determinations indicate two modes of faulting for the aftershocks. Strike-slip faulting with nodal planes striking N. 40°W. and N. 50°E. is dominant; secondary normal faulting occurs on nodal planes striking nearly north. An attempt is made to relate the strain release pattern of these aftershocks to major regional right-lateral shear and extension.
References
12
Referenced
13
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Dates
Type | When |
---|---|
Created | 4 years, 1 month ago (July 14, 2021, 1:15 p.m.) |
Deposited | 4 years, 1 month ago (July 14, 2021, 1:15 p.m.) |
Indexed | 1 year, 7 months ago (Jan. 9, 2024, 6:46 a.m.) |
Issued | 56 years, 11 months ago (Oct. 1, 1968) |
Published | 56 years, 11 months ago (Oct. 1, 1968) |
Published Online | 56 years, 11 months ago (Oct. 1, 1968) |
Published Print | 56 years, 11 months ago (Oct. 1, 1968) |
@article{Greensfelder_1968, title={Aftershocks of the Truckee, California, earthquake of September 12, 1966}, volume={58}, ISSN={0037-1106}, url={http://dx.doi.org/10.1785/bssa0580051607}, DOI={10.1785/bssa0580051607}, number={5}, journal={Bulletin of the Seismological Society of America}, publisher={Seismological Society of America (SSA)}, author={Greensfelder, Roger}, year={1968}, month=oct, pages={1607–1620} }