Retardations in fault creep rates before local moderate earthquakes along the San Andreas fault system, central California

Author:

Burford Robert O.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference31 articles.

1. Bakun, W. H., Clark, M. M., Cockerham, R. S., Ellsworth, W. L., Lindh, A. G., Prescott, W. H., Shakal, A. F., andSpudich, P. (1984),The 1984 Morgan Hill, California, earthquake. Science225, 288?291.

2. Bilham, R. G. andBeavan R. J. (1979),Strains and tilts on crustal blocks. Tectonophysics,52, 121?138.

3. Brown, R. D., Jr. (1970),Map showing recently active breaks along the San Andreas and related faults between the northern Gabilan Range and Cholame Valley, California. U.S.G.S. Misc. Geol. Inves. Map I-575, scale 1:62,500.

4. Brown, R. D., Jr. andWallace, R. E. (1968),Current and historic movement along the San Andreas fault between Paicines and Camp Dix, California. InProceedings of Conference on Geologic Problems of San Andreas Fault System (Wm. R. Dickenson and Arthur Grantz, eds) (Stanford Univ. Pub. Geol. Sci.XI) pp. 22?41.

5. Burford, R. O. (1972),Continued slip on the Coyote Creek fault after the Borrego Mountain earthquake. InThe Borrego Mountain Earthquake of Apil 9, 1968 (U.S.G.S. Prof. Paper 787) pp. 105?111.

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