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Granitic magmas residing at high levels in the continental crust may be subjected to stress transients on a wide range of time-scales. The origins of the stress transients may be internal, deriving from the volume evolution of the magmatic system, or external such as the rapid release of stresses during tectonic and volcanically derived earthquakes. The strain response of the granitic magma is cri...

The Brittle-Ductile Transition in High-Level Granitic Magmas: Material Constraints