Source time functions of large Mexican subduction earthquakes, morphology of the Benioff Zone, age of the plate, and their tectonic implications-Reference-Cited by-同舟云学术

Source time functions of large Mexican subduction earthquakes, morphology of the Benioff Zone, age of the plate, and their tectonic implications

Published:1991-12-10 Issue:B13 Volume:96 Page:21487-21502
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Singh S. K.,Mortera F.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jb/v096/iB13/91JB02047/91JB02047.pdf

Reference63 articles.

1. Strong ground motion and source mechanism of the Mexico earthquake of September 19, 1985 (Ms = 8.1);Anderson;Science,1986

2. Seismic strain release in the Mexican subduction thrust;Anderson;Phys. Earth Planet. Inter.,1989

3. An earthquake doublet in Ometepec, Guerrero, Mexico;Astiz;Phys. Earth Planet. Inter.,1984

4. Source characteristics of the earthquakes in the Michoacan seismic gap in Mexico;Astiz;Bull. Seismol. Soc. Am.,1987

5. Source mechanisms of the June 7, 1982 Ometepec, Mexico earthquakes;Beroza;Geophys. Res. Lett.,1984

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