Late Devonian syenitic intrusion from southeastern Alaska: Petrogenesis, tectonic implications, and rare metal metallogeny

The Late Devonian Corner Bay pluton is a part of the Sitkoh alkaline plutonic complex on the Chichagof Island, southeastern Alaska, which is located in the Alexander terrane of the North American Cordillera. The intrusion, about 12 km long and 4 km wide, is composed predominantly of amphibole-biotite-bearing syenitic/monzonitic rocks with minor alkaline gabbros and has a U-Pb zircon age of similar to 367 Ma interpreted as the crystallization age of the pluton. The rocks are metaluminous and have silica contents ranging from 47 to 63 wt% with a silica gap at 52-58 wt% and have high contents of alkalis, typical of shoshonitic rocks. They are rich in large-ion-lithophile elements (including Rb, Sr, Ba, U) and their isotopic composition is characterized by relatively uniform epsilon(Nd)(t) values (+3.4 to +3.7), Neoproterozoic Nd depleted mantle model ages (650-700 Ma) and initial Sr-87/Sr-86 ratios (similar to 0.704). The rocks were generated by fractional crystallization of alkali basaltic magma formed by partial melting of an amphibole-phlogopite-bearing peridotite of the sub-arc lithospheric mantle. The mantle-source underwent a Neoproterozoic metasomatic enrichment event and does not show a contribution from juvenile Devonian mantle indicating that rifting associated with the magma emplacement was of limited extent as it did not replace the old lithospheric mantle. Several geothermobarometers document emplacement of the parental magma at mid-crustal levels (8.5-10 kb) and polybaric crystallization from similar to 1200 degrees C to solidus. Crystallization of amphibole took place at similar to 880-980 degrees C and 2.4-5.5 kb. Subsequently the rocks underwent recrystallization (feld-spars: 170 Ma-40Ar/39Ar age) and re-equilibration (biotite: 129 Ma (40Ar/39Ar) at similar to 600-650 degrees C and 2 kb). Zircon, rutile and apatite saturation temperatures provide consistent results (similar to 800 degrees C). The intrusion is a part of a metallogenic province of rare metals, which stretched across the islands in the southeastern most part of Alaska. (C) 2021 Elsevier B.V. All rights reserved.

Automated summary

The Late Devonian Corner Bay pluton on Chichagof Island in southeastern Alaska is composed mainly of amphibole-biotite-bearing syenitic/monzonitic rocks with a U-Pb zircon age of around 367 Ma. The rocks are rich in large-ion-lithophile elements and have stable isotopic compositions. They were formed by fractional crystallization of alkali basaltic magma, derived from partial melting of amphibole-phlogopite-bearing peridotite undergoing Neoproterozoic metasomatism, indicating limited rifting associated with the magma emplacement.