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Science 9 April 1993: Vol. 260. no. 5105, pp. 171 - 176 DOI: 10.1126/science.260.5105.171
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Articles
Near-Field Investigations of the Landers Earthquake Sequence, April to July 1992
Kerry Sieh 1,
Lucile Jones 2,
Egill Hauksson 1,
Kenneth Hudnut 2,
Donna Eberhart-Phillips 2,
Thomas Heaton 2,
Susan Hough 2,
Kate Hutton 1,
Hiroo Kanamori 1,
Anne Lilje 1,
Scott Lindvall 3,
Sally F. McGill 4,
James Mori 2,
Charles Rubin 5,
James A. Spotila 1,
Joann Stock 1,
Hong Kie Thio 1,
Jerome Treiman 6,
Brian Wernicke 1, and
Judith Zachariasen 1
1 Seismological Laboratory 252-21, California Institute of Technology, Pasadena, CA 91125
2 U.S. Geological Survey, Pasadena, CA 91106
3 Lindvall Richter Benuska Associates, Los Angeles, CA 90041
4 Department of Geological Sciences, California State University, San Bernardino, CA 92407
5 Central Washington State University, Ellensburg, WA 98926
6 California Division of Mines and Geology, Los Angeles, CA 90012
The Landers earthquake, which had a moment magnitude (Mw) of 7.3, was the largest earthquake to strike the contiguous United States in 40 years. This earthquake resulted from the rupture of five major and many minor right-lateral faults near the southern end of the eastern California shear zone, just north of the San Andreas fault. Its Mw 6.1 preshock and Mw 6.2 aftershock had their own aftershocks and foreshocks. Surficial geological observations are consistent with local and far-field seismologic observations of the earthquake. Large surficial offsets (as great as 6 meters) and a relatively short rupture length (85 kilometers) are consistent with seismological calculations of a high stress drop (200 bars), which is in turn consistent with an apparently long recurrence interval for these faults.
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84, 817-825
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Bulletin of the Seismological Society of America
84, 835-843
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Bulletin of the Seismological Society of America
84, 844-853
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84, 863-891
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84, 892-899
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84, 917-934
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