Is there any method to know how strain at deep seated fault is ultimately transmitted to the surface?

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Oualid Melouah

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

Carlos Reinoza

Maybe the reponse is associated to geodetical methods (GNSS, INSar).

http://www.youtube.com/watch?v=SO25yVJzS1w

Stefano Cremonini

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.