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The Mount Eve granite suite is a postorogenic, A-type granitoid suite that consists of several small plutonic bodies occurring in the northwestern New Jersey–Hudson Highlands. Mount Eve granite suite rocks are equigranular, medium- to coarse-grained, quartz monzonite to granite, consisting of quartz, microperthite, and oligo-clase, with minor hornblende, biotite, and accessory zircon, apatite, titanite, magnetite, and ilmenomagnetite. Whole-rock analyses indicate that Mount Eve granite is meta-luminous to slightly peraluminous (ASI or aluminum saturation index, A/CNK or Al2O3/(CaO + Na2O + K2O) = 0.62 to 1.12) and has A-type compositional affinity defined by...

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