GARNET-BEARING GRANITIC PLUTON IN A COLLISIONAL TERRANE SUTURE ZONE, NORTHERN TALKEETNA MOUNTAINS, SOUTH-CENTRAL ALASKA
The garnet-bearing dikes and host granite are peraluminous, high K calc-alkaline, and transitional between S- and A-type granites. They also have low to moderate chondrite-normalized light rare earth element enrichment and primitive-mantle normalized enrichment in some large ion lithophile elements and depletion of Ba, Sr, Eu, and Ti (consistent with fractional crystallization of plagioclase and Fe-Ti oxides). The granitic host is geochemically similar to other collisional igneous rocks in the WCT suture zone and is consistent with a model in which granitic magmas formed by assimilation-fractional crystallization from an enriched mafic source that partially melted and assimilated aluminum-rich crustal rocks of the suture zone (Kahiltna assemblage flysch). The garnet-bearing dikes represent small volumes of late-stage magma that formed as partial melts of Kahiltna flysch, yielding modal garnet and muscovite, and releasing fluids which contributed to the formation of the myrmekite and graphic textures either as exsolution or metasomatic reactions. The granitic pluton and garnet-bearing granitic dikes confirm an episode of collisional magmatism in the WCT suture zone that involved partial melting of upper- to mid-level sedimentary crustal rocks.