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The aftershocks were processed using HYPO71 (Lee and Valdes, 1985) for the hypocenter determination.
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The aftershocks were starting to be felt.
The aftershocks were less frequent and less powerful.
The aftershock is used for testing velocity structure models.
The aftershocks are ongoing and making people very nervous".
The aftershocks are represented by open circles.
The aftershocks are classified by their depths.
Still, the aftershock was felt all day.
The aftershock was felt between the Valparaíso and Maule regions.
The spatial extent of aftershocks is used to estimate the source fault location.
The aftershock distribution was determined using the estimated local velocity structure.
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