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High-pressure granulite facies metamorphism (1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A
by
Ague, Jay J
, Keller, Duncan S
in
Acadian Phase
/ alkali feldspar
/ Bigelow Brook Formation
/ Biotite
/ Brimfield Schist
/ Central Maine Terrane
/ chemical composition
/ Colour
/ Connecticut
/ Corundum
/ Crystallography
/ Crystals
/ Devonian
/ Domains
/ Eclogite
/ eclogite facies
/ facies
/ feldspar group
/ Feldspars
/ felsic composition
/ framework silicates
/ Garnet
/ garnet group
/ Garnets
/ geologic thermometry
/ Gneiss
/ gneisses
/ granulite facies
/ granulites
/ high pressure
/ high-grade metamorphism
/ High-pressure granulite
/ igneous and metamorphic rocks
/ igneous rocks
/ Ilmenite
/ Inclusions
/ K-feldspar
/ Kimberlites
/ Kyanite
/ Lamellae
/ leucosomes
/ Magma
/ Maine
/ Melting
/ metamorphic rocks
/ Metamorphism
/ Metamorphism (geology)
/ mica group
/ migmatites
/ Mineral assemblages
/ Minerals
/ nesosilicates
/ Organic chemistry
/ orogenic belts
/ Orogeny
/ orthosilicates
/ oxides
/ P-T conditions
/ Paleoproterozoic
/ Paleozoic
/ paragenesis
/ perthite
/ Petrology
/ phase diagrams
/ phase equilibria
/ Phosphorus pentoxide
/ Plagioclase
/ plutonic rocks
/ Precambrian
/ Pressure
/ Proterozoic
/ pseudomorphism
/ Rock
/ Rocks
/ Sapphire
/ Schist
/ Schists
/ Sedimentary facies
/ Shades
/ sheet silicates
/ Silica
/ silica-undersaturated
/ silicates
/ Silicon dioxide
/ Sillimanite
/ Spinel
/ Subduction
/ Subduction (geology)
/ Subduction zones
/ syenite
/ syenites
/ tectonics
/ terranes
/ United States
/ upper Precambrian
/ xenoliths
2018
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High-pressure granulite facies metamorphism (1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A
by
Ague, Jay J
, Keller, Duncan S
in
Acadian Phase
/ alkali feldspar
/ Bigelow Brook Formation
/ Biotite
/ Brimfield Schist
/ Central Maine Terrane
/ chemical composition
/ Colour
/ Connecticut
/ Corundum
/ Crystallography
/ Crystals
/ Devonian
/ Domains
/ Eclogite
/ eclogite facies
/ facies
/ feldspar group
/ Feldspars
/ felsic composition
/ framework silicates
/ Garnet
/ garnet group
/ Garnets
/ geologic thermometry
/ Gneiss
/ gneisses
/ granulite facies
/ granulites
/ high pressure
/ high-grade metamorphism
/ High-pressure granulite
/ igneous and metamorphic rocks
/ igneous rocks
/ Ilmenite
/ Inclusions
/ K-feldspar
/ Kimberlites
/ Kyanite
/ Lamellae
/ leucosomes
/ Magma
/ Maine
/ Melting
/ metamorphic rocks
/ Metamorphism
/ Metamorphism (geology)
/ mica group
/ migmatites
/ Mineral assemblages
/ Minerals
/ nesosilicates
/ Organic chemistry
/ orogenic belts
/ Orogeny
/ orthosilicates
/ oxides
/ P-T conditions
/ Paleoproterozoic
/ Paleozoic
/ paragenesis
/ perthite
/ Petrology
/ phase diagrams
/ phase equilibria
/ Phosphorus pentoxide
/ Plagioclase
/ plutonic rocks
/ Precambrian
/ Pressure
/ Proterozoic
/ pseudomorphism
/ Rock
/ Rocks
/ Sapphire
/ Schist
/ Schists
/ Sedimentary facies
/ Shades
/ sheet silicates
/ Silica
/ silica-undersaturated
/ silicates
/ Silicon dioxide
/ Sillimanite
/ Spinel
/ Subduction
/ Subduction (geology)
/ Subduction zones
/ syenite
/ syenites
/ tectonics
/ terranes
/ United States
/ upper Precambrian
/ xenoliths
2018
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High-pressure granulite facies metamorphism (1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A
by
Ague, Jay J
, Keller, Duncan S
in
Acadian Phase
/ alkali feldspar
/ Bigelow Brook Formation
/ Biotite
/ Brimfield Schist
/ Central Maine Terrane
/ chemical composition
/ Colour
/ Connecticut
/ Corundum
/ Crystallography
/ Crystals
/ Devonian
/ Domains
/ Eclogite
/ eclogite facies
/ facies
/ feldspar group
/ Feldspars
/ felsic composition
/ framework silicates
/ Garnet
/ garnet group
/ Garnets
/ geologic thermometry
/ Gneiss
/ gneisses
/ granulite facies
/ granulites
/ high pressure
/ high-grade metamorphism
/ High-pressure granulite
/ igneous and metamorphic rocks
/ igneous rocks
/ Ilmenite
/ Inclusions
/ K-feldspar
/ Kimberlites
/ Kyanite
/ Lamellae
/ leucosomes
/ Magma
/ Maine
/ Melting
/ metamorphic rocks
/ Metamorphism
/ Metamorphism (geology)
/ mica group
/ migmatites
/ Mineral assemblages
/ Minerals
/ nesosilicates
/ Organic chemistry
/ orogenic belts
/ Orogeny
/ orthosilicates
/ oxides
/ P-T conditions
/ Paleoproterozoic
/ Paleozoic
/ paragenesis
/ perthite
/ Petrology
/ phase diagrams
/ phase equilibria
/ Phosphorus pentoxide
/ Plagioclase
/ plutonic rocks
/ Precambrian
/ Pressure
/ Proterozoic
/ pseudomorphism
/ Rock
/ Rocks
/ Sapphire
/ Schist
/ Schists
/ Sedimentary facies
/ Shades
/ sheet silicates
/ Silica
/ silica-undersaturated
/ silicates
/ Silicon dioxide
/ Sillimanite
/ Spinel
/ Subduction
/ Subduction (geology)
/ Subduction zones
/ syenite
/ syenites
/ tectonics
/ terranes
/ United States
/ upper Precambrian
/ xenoliths
2018
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High-pressure granulite facies metamorphism (1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A
Journal Article
High-pressure granulite facies metamorphism (1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A
2018
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Overview
We quantify the metamorphic pressure-temperature (P-T) conditions for a newly discovered silica-undersaturated high-pressure granulite (HPG) from the Central Maine Terrane (CMT) in northeastern Connecticut, U.S.A. The rocks lie within the Acadian-Neoacadian orogenic belt (Devonian) and form part of the Brimfield Schist. The Brimfield and the adjacent Bigelow Brook Formation contain silica-saturated rocks that have previously been shown to have undergone ∼1000 °C metamorphism. The pressure was less well constrained at ≥ ∼1 GPa. Silica-undersaturated rocks hold underutilized potential for pinpointing peak metamorphic conditions, particularly pressure, because of their resilience to melting and the variety of refractory minerals they contain. The typical silica-undersaturated mineral assemblage is garnet + spinel + corundum + plagioclase + K-feldspar + biotite + ilmenite. Leucosomes are syenites consisting of two feldspars ± biotite. Plagioclase is commonly antiperthitic, particularly in feldspathic domains surrounding peritectic garnet; such garnet crystals reach ∼10 cm in diameter. Alkali feldspars are perthitic. The rocks contain remarkable ellipsoidal spinels as much as 5.5 cm long comprising discrete crystallographic domains hosting crystallographically oriented lamellae of a Fe-Ti phase, most likely ilmenite. Corundum is usually colorless, but can also be found as sapphire in shades of pink, purple, and blue, particularly in antiperthite-rich domains surrounding large garnets. Some sapphires are concentrically color zoned. We carried out a P-T estimation using ternary feldspar reintegration thermometry of metamorphic antiperthites together with pseudosection modeling. Samples texturally and chemically record near-eclogite facies equilibration at minimum conditions of ∼1040 °C and ∼1.8 GPa, establishing the CMT in northeastern CT as the first known HPG locality in the U.S. These results are consistent with high P2O5 levels found in garnet (0.18 wt%), Ti-in-biotite thermometry, regional sillimanite pseudomorphs after kyanite, and preliminary experimental work on melt inclusions in garnet (Ferrero et al. 2017). The leucosomes provide strong evidence that partial melting of silica-undersaturated rocks at HPG conditions can produce syenitic magmata. Strongly melt-depleted silica-undersaturated rocks may also be protoliths for garnet + spinel + corundum xenoliths reported from kimberlites. The presence of HPG gneisses demonstrates that the large-scale thrusts of the CMT sample the deepest roots of the orogenic belt (60-70 km), and perhaps even deeper subduction zone lithologies as well.
Publisher
Mineralogical Society of America,Walter de Gruyter GmbH
Subject
/ Biotite
/ Colour
/ Corundum
/ Crystals
/ Devonian
/ Domains
/ Eclogite
/ facies
/ Garnet
/ Garnets
/ Gneiss
/ gneisses
/ igneous and metamorphic rocks
/ Ilmenite
/ Kyanite
/ Lamellae
/ Magma
/ Maine
/ Melting
/ Minerals
/ Orogeny
/ oxides
/ perthite
/ Pressure
/ Rock
/ Rocks
/ Sapphire
/ Schist
/ Schists
/ Shades
/ Silica
/ Spinel
/ syenite
/ syenites
/ terranes
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