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The '''1965 Oaxaca earthquake''' occurred in ] on August 23, 1965 at 13:46 (19:46 ]). It was an ] with magnitude ] 7.5.<ref>E. Chael, G. Stewart, "Recent large earthquakes along the Middle America trench and their implications for the subduction process"</ref><ref>A. Iglesias, S. K. Singh, M. Ordaz, M. A. Santoyo, J. Pacheco, "The seismic alert system for Mexico City: An evaluation of performance and a strategy for its improvement"</ref> 5 people were reported dead in ] and 1 in ]. There was an anomalous change in seismic activities before the earthquake. There was a quiescent stage from late 1963 to mid-1964, and it was followed by a renewal of seismic activities before the main shock.<ref>http://www.zisin.geophys.tohoku.ac.jp/ohtake/ohtake1-20.pdf</ref> This earthquake was a shallow thrust earthquake in the interplate ] zone, in which the ] is subducting beneath the ].<ref>http://www.geology.wisc.edu/~chuck/PDF/FCM_Oax_GJI08.pdf</ref><ref>http://www.eri.u-tokyo.ac.jp/seno/Papers/epsl_kato_seno.pdf</ref> |
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The '''1965 Oaxaca earthquake''' occurred in ] on August 23 at {{tooltip|13:46|19:46 UTC]]}} with a ] of 7.5.<ref>E. Chael, G. Stewart, "Recent large earthquakes along the Middle America trench and their implications for the subduction process"</ref><ref>A. Iglesias, S. K. Singh, M. Ordaz, M. A. Santoyo, J. Pacheco, "The seismic alert system for Mexico City: An evaluation of performance and a strategy for its improvement"</ref> Five people were reported dead in ] and 1 in ]. There was an anomalous change in seismic activities before the earthquake. There was a quiescent stage from late 1963 to mid-1964, and it was followed by a renewal of seismic activities before the main shock.<ref>{{citation|title=Seismicity gap near Oaxaca, southern Mexico as a probable precursor to a large earthquake|url=http://www.zisin.geophys.tohoku.ac.jp/ohtake/ohtake1-20.pdf|first=M.|last=Ohtake|first2=T.|last2=Matumoto|first3=Gary|last3=Latham|year=1977|journal=Pure and Applied Geophysics|publisher=]|volume=115|pages=375–385}}</ref> This earthquake was a shallow thrust earthquake in the interplate ] zone, in which the ] is subducting beneath the ].<ref>http://www.geology.wisc.edu/~chuck/PDF/FCM_Oax_GJI08.pdf</ref><ref>http://www.eri.u-tokyo.ac.jp/seno/Papers/epsl_kato_seno.pdf</ref> |