Geology Reference
In-Depth Information
Figure 9.7
Localised shearing at contact between mafic enclave and granite
host. Fabric intensity drops off away from the enclave margin and is absent in
the body of the host granite, implying a synmagmatic origin.
Figure 9.8
Parallel-striking synplutonic dykes of basaltic andesite cutting gra-
nodiorite that was only partially crystallised, Coastal Batholith, Peru.
