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Study of the structural changes in the Popocatepetl volcano in Mexico related to microseismicity by applying the lineament analysis to the Aster (Terra) satellite data

2007/06/13 by A. A. Arellano-Baeza, R. V. García, Arellano-Baeza, A. A. +5
Earth and Planetary Sciences · Physics and Astronomy · #FOS: Physical sciences #Geological and Tectonic Studies in Latin America #Geophysics (physics.geo-ph) #Seismic Waves and Analysis #earthquake and tectonic studies #physics.geo-ph

paper · pdf · doi:10.48550/arxiv.0706.1814

Submitted to Advances in Space Research

arxiv created 2007/06/13 · openalex publication_date 2007/06/13 · arxiv updated 2009/12/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/28

Abstract

Mexico is one of the most volcanically active regions in North America. Volcanic activity in central Mexico is associated with the subduction of the Cocos and Rivera plates beneath the North American plate. Periods of enhanced microseismic activity, associated with the volcanic activity of the Popocatepetl volcano is compared with periods, during which the microseismic activity was low. We detected systematical changes in the number of lineaments, associated with the microseismic activity due to lineament analysis of a temporal sequence of high resolution satellite images of the Popocatepetl volcano, provided by the ASTER/VNIR instrument. The Lineament Extraction and Stripes Statistic Analysis (LESSA) software package was used for the lineament extraction. In the future it would allow develop a methodology for detection of possible elevation of pressure in volcano edifice.

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