Rupture characteristics of M7.2 Sierra El Mayor (Mexico) earthquake
The April 4, 2010 "Easter Sunday" earthquake ruptured several NW trending faults in the Sierra Cupapa - Sierra El Mayor mountain range to the west of Laguna Salada.
Ascending track 211, Jan 15 2010 - Apr 17
2010 (preliminary orbits, perperdicular baseline of 700 m). Color
fringes indicate changes in the radar range (one color cycle
corresponding to 11.8 cm of line-of-sight displacement). Black wavy
lines denote the geologically mapped rupture
trace.
Interferometric correlation
Same pair as above. Color
denotes variations in radar correlation. Zones of low correlation
(red areas) denote significant changes in reflective properties of
the ground. Note a wide fault zone in the Cupapa mountains and
extensive decorrelation in the agricultural area to the east of the
rupture (possibly due to extensive liquefaction).
Coseismic interferogram - ENVISAT
Ascending track 306, Mar 9 2010 - Apr 13 2010
(preliminary orbits, perperdicular baseline of 270 m). Color fringes
indicate changes in the radar range (one color cycle corresponding to
2.8 cm of line-of-sight displacement). Note a northern termination of
rupture just past the US-Mexico border. Black wavy lines denote the
geologically mapped rupture
trace.
Interferometric correlation
Same pair as above. Color
denotes variations in radar correlation. Zones of low correlation
(red areas) denote significant changes in reflective properties of
the ground. Note a wide fault zone in the Cupapa mountains and
extensive decorrelation in the agricultural area to the east of the
rupture (possibly due to extensive liquefaction).
Preseismic interferogram - ENVISAT
ENVISAT, Nov 24 2009 - Mar 9 2010, ascending track
306. Color fringes indicate changes in the radar range (one color
cycle corresponding to 2.8 cm of line-of-sight displacement). Black
wavy lines denote the geologically mapped rupture trace.
Fault slip model (soon)