Hello everybody.
I recently worked in some zones of the western Alps where crop out fault
zones with a complex evolutionary history for the rheological aspects. The
most interesting feature of these fault zones is that in many cases a
brittle deformation event related to the development of cataclastic flow
seem to be followed locally by a ductile deformation imposed by the
incoming in the shear zones of fluids related to ore deposition.
I would like to know if somebody knows recent works which deal with this
kind of deformation.
Thank You everybody,
Paolo.
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