The 1997–1998 Activity of Volcán de Colima,Western Mexico: Some Aspects of the Associated Seismic Activity |
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Authors: | Araceli Zamora-Camacho Juan Manuel Espíndola Gabriel Reyes-Dávila |
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Institution: | (1) Instituto de Geofisica, UNAM, Av. Universidad 3000, Coyoacán, D.F, 04510, Mexico;(2) Observatorio Vulcanológico,Universidad de Colima, Av. Gonzalo de Sandoval No. 333, Col. Las Víboras, 28052, Colima, Mexico |
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Abstract: | Volcán de Colima, the most active volcano in Mexico, had a climactic episode on 20 November, 1998. On this date, a dome formed
on the small summit crater during the previous few days, collapsed generating block-and-ash flows. The event was preceded
by almost twelve months of seismic activity, which continued afterwards for several more months. We analyzed the main seismic
activity, which occurred from 20 March, 1998 to 31 March, 1999. The seismicity was dominated by volcano-tectonic earthquakes
before the climax, and subsequently by hybrid and long-period earthquakes. We determined the frequency of events for the entire
period, and located most of the volcano-tectonic events. To assess the possibility that these earthquakes were generated by
the same source, they were tested for their similitude through cross correlation in the time domain. Six groups of similar
events, or earthquake families, were generated. The members of these families appeared before the 20 November event, apparently
ceasing afterwards. We examined the location of the families' events with respect to an existing gravity model in which an
anomalous body of negative density contrast suggests the presence of the magma chamber. Most of the family events occur on
top of the anomalous body, which suggests they were associated with the passage of magma through the feeding conduits of the
volcano. |
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Keywords: | Colima volcano Mexican volcanoes volcano seismicity seismicity in andesitic volcanoes similar earthquakes earthquake families |
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