Dg. Quirk et al., Insights into the collection and emplacement of granitic magma based on 3Dseismic images of normal fault-related salt structures, TERRA NOVA, 10(5), 1998, pp. 268-273
3D seismic data from salt structures in the Southern North Sea show how vis
cous fluids tend to migrate towards and flow upwards along the footwalls of
active normal faults where zones of low stress are inherent. This process
provides one potential solution for the question of how enough space is tre
ated to accommodate large granitic bodies in the crust. During episodes of
regional extension, granitic melt may collect in the lower crust below norm
al detachments in domed areas from which magma may be sourced. Subsequently
, in the upper crust, emplacement can occur in fault-bounded laccoliths at
rates commensurate with other geological processes.