Are A‐type granites the high‐temperature felsic granites? Evidence from fractionated granites of the Wangrah Suite

A‐type granites are a minor, but distinctive, component of the granites of the Lachlan Fold Belt of southeastern Australia. They are felsic rocks with SiO2 contents ranging from 69.7 to 77.1%, with an average of 73.8% (55 analyses). When unfractionated, as evidenced by high Ba contents, they are dis... View More