Does ternary feldspar constrain the metamorphic conditions of high‐grade meta‐igneous rocks? Evidence from orthopyroxene granulites, Bohemian Massif
Identifieur interne : 002E07 ( Istex/Corpus ); précédent : 002E06; suivant : 002E08Does ternary feldspar constrain the metamorphic conditions of high‐grade meta‐igneous rocks? Evidence from orthopyroxene granulites, Bohemian Massif
Auteurs : P. Štípská ; R. PowellSource :
- Journal of Metamorphic Geology [ 0263-4929 ] ; 2005-10.
English descriptors
- KwdEn :
- American mineralogist, Anorthite, Antiperthite, Antiperthite grains, Antiperthite inclusions, Assemblage, Biotite, Blackwell publishing, Bohemian, Bohemian massif, Carswell, Clinopyroxene, Compositional, Coronitic garnet, Crustal, Crystallization, Crystallization interval, Czech, Czech republic, Decompression, Earth sciences, Eclogites, Eld, Elkins grove, European journal, Exsolution, Facies, Feldspar, Felsic, Felsic matrix, Fiala, Fuhrman, Fuhrman lindsley, Garnet, Garnet growth, Garnet incl, Garnet proportion, Garnet zoning, Gfohl unit, Granulite, Granulite massifs, Granulites, Grossular, Grossular content, Growth zoning, High grossular content, High temperature, Holland powell, Hydrous, Igneous, Igneous crystallization, Igneous protolith, Inclusion, Isopleth, Jawecki, Kbar, Krone, Lamella, Lindsley, Lower austria, Lower pressure, Lower temperature, Magma, Magmatic, Magmatic rocks, Massif, Matrix, Metamorphic, Metamorphic conditions, Metamorphic geology, Metamorphic history, Metamorphic origin, Metamorphic peak, Metamorphic rocks, Metamorphism, Mineral assemblage, Mineral assemblages, Mineralogist, Moldanubian, Moldanubian granulites, Moldanubian zone, Muscovite, Orthopyroxene, Orthopyroxene granulites, Owen dostal, Peak pressure, Perthite, Petrakakis, Petrakakis jawecki, Petrology, Phase diagrams, Plagioclase, Plagioclase host, Pressure peak, Primary interest, Prograde, Prograde garnet, Prograde metamorphism, Prograde path, Pseudosection, Pseudosections, Quartz, Recrystallization, Reintegration, Relict, Rock composition, Rotzler, Solidus, Solidus temperature, Ternary, Ternary feldspar, Ternary feldspar grain, Ternary feldspar grains, Variscan, Vrana, Zircon, Zircon ages.
- Teeft :
- American mineralogist, Anorthite, Antiperthite, Antiperthite grains, Antiperthite inclusions, Assemblage, Biotite, Blackwell publishing, Bohemian, Bohemian massif, Carswell, Clinopyroxene, Compositional, Coronitic garnet, Crustal, Crystallization, Crystallization interval, Czech, Czech republic, Decompression, Earth sciences, Eclogites, Eld, Elkins grove, European journal, Exsolution, Facies, Feldspar, Felsic, Felsic matrix, Fiala, Fuhrman, Fuhrman lindsley, Garnet, Garnet growth, Garnet incl, Garnet proportion, Garnet zoning, Gfohl unit, Granulite, Granulite massifs, Granulites, Grossular, Grossular content, Growth zoning, High grossular content, High temperature, Holland powell, Hydrous, Igneous, Igneous crystallization, Igneous protolith, Inclusion, Isopleth, Jawecki, Kbar, Krone, Lamella, Lindsley, Lower austria, Lower pressure, Lower temperature, Magma, Magmatic, Magmatic rocks, Massif, Matrix, Metamorphic, Metamorphic conditions, Metamorphic geology, Metamorphic history, Metamorphic origin, Metamorphic peak, Metamorphic rocks, Metamorphism, Mineral assemblage, Mineral assemblages, Mineralogist, Moldanubian, Moldanubian granulites, Moldanubian zone, Muscovite, Orthopyroxene, Orthopyroxene granulites, Owen dostal, Peak pressure, Perthite, Petrakakis, Petrakakis jawecki, Petrology, Phase diagrams, Plagioclase, Plagioclase host, Pressure peak, Primary interest, Prograde, Prograde garnet, Prograde metamorphism, Prograde path, Pseudosection, Pseudosections, Quartz, Recrystallization, Reintegration, Relict, Rock composition, Rotzler, Solidus, Solidus temperature, Ternary, Ternary feldspar, Ternary feldspar grain, Ternary feldspar grains, Variscan, Vrana, Zircon, Zircon ages.
Abstract
The presence of ternary feldspar in high‐grade meta‐igneous rocks, and the recognition of the thermometric significance of this mineral, has led recent researchers to postulate peak metamorphic temperatures in excess of 1000 °C. However, it needs to be established that such ternary feldspar is not in fact a survivor of the original high‐temperature crystallization of the igneous protolith. After exsolution, the host and lamellae in the ternary feldspar grains may be stable throughout subsequent history as long as recrystallization does not occur. Such a history may involve rehydration and metamorphism, including H2O‐saturated conditions, with the compositions and proportions of the host and lamellae being modified to reflect the P–T conditions experienced. In the case of the high‐grade meta‐igneous rocks from the Moldanubian of the Bohemian Massif, some samples that contain ternary feldspar preserve a substantial measure of their igneous heritage. Orthopyroxene‐bearing granulites not only include types that are barely affected by the metamorphism, but also others that have undergone hydration of the igneous protolith prior to the development of a metamorphic overprint. A key to establishing the igneous origin of the ternary feldspar grains is their preservation in garnet that is either itself igneous, or of a relatively low‐temperature metamorphic origin. Applying the logic to the other ternary feldspar‐bearing meta‐igneous rocks deprives the Moldanubian of its ultrahigh temperature (UHT) metamorphic status.
Url:
DOI: 10.1111/j.1525-1314.2005.00600.x
Links to Exploration step
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<front><div type="abstract" xml:lang="en">The presence of ternary feldspar in high‐grade meta‐igneous rocks, and the recognition of the thermometric significance of this mineral, has led recent researchers to postulate peak metamorphic temperatures in excess of 1000 °C. However, it needs to be established that such ternary feldspar is not in fact a survivor of the original high‐temperature crystallization of the igneous protolith. After exsolution, the host and lamellae in the ternary feldspar grains may be stable throughout subsequent history as long as recrystallization does not occur. Such a history may involve rehydration and metamorphism, including H2O‐saturated conditions, with the compositions and proportions of the host and lamellae being modified to reflect the P–T conditions experienced. In the case of the high‐grade meta‐igneous rocks from the Moldanubian of the Bohemian Massif, some samples that contain ternary feldspar preserve a substantial measure of their igneous heritage. Orthopyroxene‐bearing granulites not only include types that are barely affected by the metamorphism, but also others that have undergone hydration of the igneous protolith prior to the development of a metamorphic overprint. A key to establishing the igneous origin of the ternary feldspar grains is their preservation in garnet that is either itself igneous, or of a relatively low‐temperature metamorphic origin. Applying the logic to the other ternary feldspar‐bearing meta‐igneous rocks deprives the Moldanubian of its ultrahigh temperature (UHT) metamorphic status.</div>
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<author><json:item><name>P. ŠTÍPSKÁ</name>
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<abstract lang="en">The presence of ternary feldspar in high‐grade meta‐igneous rocks, and the recognition of the thermometric significance of this mineral, has led recent researchers to postulate peak metamorphic temperatures in excess of 1000 °C. However, it needs to be established that such ternary feldspar is not in fact a survivor of the original high‐temperature crystallization of the igneous protolith. After exsolution, the host and lamellae in the ternary feldspar grains may be stable throughout subsequent history as long as recrystallization does not occur. Such a history may involve rehydration and metamorphism, including H2O‐saturated conditions, with the compositions and proportions of the host and lamellae being modified to reflect the P–T conditions experienced. In the case of the high‐grade meta‐igneous rocks from the Moldanubian of the Bohemian Massif, some samples that contain ternary feldspar preserve a substantial measure of their igneous heritage. Orthopyroxene‐bearing granulites not only include types that are barely affected by the metamorphism, but also others that have undergone hydration of the igneous protolith prior to the development of a metamorphic overprint. A key to establishing the igneous origin of the ternary feldspar grains is their preservation in garnet that is either itself igneous, or of a relatively low‐temperature metamorphic origin. Applying the logic to the other ternary feldspar‐bearing meta‐igneous rocks deprives the Moldanubian of its ultrahigh temperature (UHT) metamorphic status.</abstract>
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