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Source characteristics of the 1985 Michoacan, Mexico earthquake at periods of 1 to 30 seconds

Houston, Heidi and Kanamori, Hiroo (1986) Source characteristics of the 1985 Michoacan, Mexico earthquake at periods of 1 to 30 seconds. Geophysical Research Letters, 13 (6). pp. 597-600. ISSN 0094-8276. http://resolver.caltech.edu/CaltechAUTHORS:20141112-132756765

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Abstract

Source characteristics of the Sept. 19, 1985 Michoacan, Mexico earthquake and its aftershock on Sept. 21 were inferred from broadband and short-period teleseismic GDSN records. We Fourier-transformed the P waves, corrected for instrument response, attenuation, geometrical spreading, and radiation pattern (including the depth phases), and then averaged to obtain the teleseismic source spectrum from 1 to 30 s. The Michoacan source spectrum is enriched at 30 s and depleted at 1 to 10 s relative to an average source spectrum of large interplate subduction events. Source spectra for the Sept. 21 aftershock, 1981 Playa Azul, 1979 Petatlan, and 1978 Oaxaca events follow a trend similar to that of the 1985 Michoacan event. This spectral trend may characterize the Mexican subduction zone. A station-by-station least-squares inversion of the Michoacan earthquake records for the source time function yielded three source pulses, which we interpreted as events on the fault plane. The first two are similar in moment, and the third contains only 20% of the moment of the first. Directivity is evident in the timing. At each station, we measured the time differences between the pulses, and performed a least-squares nonlinear estimation of the strike, distance, and time separation between the events to locate them relative to one another. The second event occurred 26 s after the first, and 82 km southeast of it, indicating southeastward rupture along the trench. The third event occurred 21 s after the second, and about 40 km seaward of it. The two large events are also seen in the near-field strong motions. The mainshock records, spectrum, and time functions contain less high frequency radiation than those of the 1985 Valparaiso, Chile earthquake. Apparently, the Michoacan earthquake ruptured two relatively smooth, strong patches which generated large 30 s waves, but small 1 to 10 s waves. Such behavior contrasts with the Valparaiso event which had a more complex rupture process and generated more 1 to 5 s energy. This difference is consistent with the higher near-field accelerations recorded for the Valparaiso event.


Item Type:Article
Related URLs:
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http://dx.doi.org/10.1029/GL013i006p00597DOIArticle
http://onlinelibrary.wiley.com/doi/10.1029/GL013i006p00597/abstractPublisherArticle
Additional Information:© 1986 American Geophysical Union. Received February 24, 1986; accepted April 15, 1986. Steve Hartzell helped us use his program to invert for source time functions. John Vidale and an anonymous reviewer helped improve the manuscript. This research was supported by U.S.G.S. Grant 14-08-0001-G-1170. Contribution No. 4312, Division of Geological and Planetary Sciences, California Institute of Technology.
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USGS14-08-0001-G- 1170
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Caltech Division of Geological and Planetary Sciences4312
Record Number:CaltechAUTHORS:20141112-132756765
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20141112-132756765
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:51669
Collection:CaltechAUTHORS
Deposited By: Jason Perez
Deposited On:13 Nov 2014 21:26
Last Modified:13 Nov 2014 21:26

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