with the behaviour of the zone as a left-lateral transform zone,
but the recent (Pliocene-
Quaternary) stress-field inferred from geological observations,
presumably reflects both previous behaviour of the area, at the time it was located inside
the rift zone, and its present location. These conclusions may also support the idea of the
evolution from rift kinematics to transform motion.
The mapped surface
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf