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Anomalous groundwater level and temperature changes are compared with ground deformation recorded before and after an earthquake of MW 5.4 and its foreshocks and aftershocks that occurred during 22–28 May 2006 in the Mexicali Valley, Baja California, Mexico. The coseismic groundwater level changes could be attributed to static volumetric strain changes caused by the mainshock, except for one well,...
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