The strain at depth will induced stress at subsequent shallower depth and this process will continue until it is released at the surface.
YES YOU CAN USE GRAVIMETRY BY APPLICATION OF UPWARD CONTINUATION PROCESS TO DIFFERENT DISTANCE (YOU CAN USE OASIS MONTAJ SOFT)
YOU CAN COMBINE GRAVIMETRY AND REMOTE SENSING (detection of lineament) IF ANOMLYS ARE SUPORPOSED IN THE TWO METHODS thats mean thats are contonious
Maybe the reponse is associated to geodetical methods (GNSS, INSar).
http://www.youtube.com/watch?v=SO25yVJzS1w
I don't know very well the topic but it is very interesting for me too.
In my region (Emilia, Italy) an earthquake happened in 2012 and it was and is still studied (e.g., Annals of Geophysics 55/4, 2012 and subsequent papers on international journals).
If you will search among the italian INGV (National Institute of Geophysics and volcanology) contributions you will find surely something matching your interests.
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