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The Clarence River Supersuite (CRS) is one of the three late Permian I-type supersuites in the southern New England Orogen of eastern Australia. It comprises 12 small (mostly <100 km2) intrusions that occur at the northeastern and southern extremities of the batholith. The intrusions are compositionally diverse, ranging from gabbro to monzogranite, but are dominated by tonalite, granodiorite and d...

Clarence River Supersuite: 250 Ma Cordilleran Tonalitic I-type Intrusions in Eastern Australia