Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway)
Graphite formation in the deep crust during granulite facies metamorphism is documented in the Proterozoic gneisses of the Lofoten–Vesterålen Complex, northern Norway. Graphite schist is hosted in banded gneisses dominated by orthopyroxene-bearing quartzofeldspathic gneiss, including marble, calcsil...
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ftdoajarticles:oai:doaj.org/article:de460379b168461b8abb4e17b6ccdef5 2023-11-12T04:20:41+01:00 Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway) Ane K. Engvik Håvard Gautneb Pål Tore Mørkved Janja Knežević Solberg Muriel Erambert 2023-09-01T00:00:00Z https://doi.org/10.3390/min13101279 https://doaj.org/article/de460379b168461b8abb4e17b6ccdef5 EN eng MDPI AG https://www.mdpi.com/2075-163X/13/10/1279 https://doaj.org/toc/2075-163X doi:10.3390/min13101279 2075-163X https://doaj.org/article/de460379b168461b8abb4e17b6ccdef5 Minerals, Vol 13, Iss 1279, p 1279 (2023) C-isotope fluid granulite graphite Vesterålen Mineralogy QE351-399.2 article 2023 ftdoajarticles https://doi.org/10.3390/min13101279 2023-10-29T00:36:00Z Graphite formation in the deep crust during granulite facies metamorphism is documented in the Proterozoic gneisses of the Lofoten–Vesterålen Complex, northern Norway. Graphite schist is hosted in banded gneisses dominated by orthopyroxene-bearing quartzofeldspathic gneiss, including marble, calcsilicate rocks and amphibolite. The schist has major graphite (<modality 39%), quartz, plagioclase, pyroxenes, biotite (Mg# = 0.67–0.91; Ti < 0.66 a.p.f.u.) and K-feldspar/perthite. Pyroxene is orthopyroxene (En 69–74 ) and/or clinopyroxene (En 33–53 Fs 1–14 Wo 44–53 ); graphite occurs in assemblage with metamorphic orthopyroxene. Phase diagram modelling (plagioclase + orthopyroxene (Mg#-ratio = 0.74) + biotite + quartz + rutile + ilmenite + graphite-assemblage) constrains pressure-temperature conditions of 810–835 °C and 0.73–0.77 GPa; Zr-in-rutile thermometry 726–854 °C. COH fluids stabilise graphite and orthopyroxene; the high Mg#-ratio of biotite and pyroxenes, and apatite Cl < 2 a.p.f.u., indicate the importance of fluids during metamorphism. Stable isotopic δ 13 C graphite in the graphite schist is −38 to −17‰; δ 13 C calcite of marbles +3‰ to +10‰. Samples with both graphite and calcite present give lighter values for δ 13 C calcite = −8.7‰ to −9.5‰ and heavier values for δ 13 C graphite = −11.5‰ to −8.9‰. δ 18 O calcite for marble shows lighter values, ranging from −15.4‰ to −7.5‰. We interpret the graphite origin as organic carbon accumulated in sediments, while isotopic exchange between graphite and calcite reflects metamorphic and hydrothermal re-equilibration. Article in Journal/Newspaper Lofoten Northern Norway Vesterålen Directory of Open Access Journals: DOAJ Articles Minerals 13 10 1279 |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
C-isotope fluid granulite graphite Vesterålen Mineralogy QE351-399.2 |
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C-isotope fluid granulite graphite Vesterålen Mineralogy QE351-399.2 Ane K. Engvik Håvard Gautneb Pål Tore Mørkved Janja Knežević Solberg Muriel Erambert Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway) |
topic_facet |
C-isotope fluid granulite graphite Vesterålen Mineralogy QE351-399.2 |
description |
Graphite formation in the deep crust during granulite facies metamorphism is documented in the Proterozoic gneisses of the Lofoten–Vesterålen Complex, northern Norway. Graphite schist is hosted in banded gneisses dominated by orthopyroxene-bearing quartzofeldspathic gneiss, including marble, calcsilicate rocks and amphibolite. The schist has major graphite (<modality 39%), quartz, plagioclase, pyroxenes, biotite (Mg# = 0.67–0.91; Ti < 0.66 a.p.f.u.) and K-feldspar/perthite. Pyroxene is orthopyroxene (En 69–74 ) and/or clinopyroxene (En 33–53 Fs 1–14 Wo 44–53 ); graphite occurs in assemblage with metamorphic orthopyroxene. Phase diagram modelling (plagioclase + orthopyroxene (Mg#-ratio = 0.74) + biotite + quartz + rutile + ilmenite + graphite-assemblage) constrains pressure-temperature conditions of 810–835 °C and 0.73–0.77 GPa; Zr-in-rutile thermometry 726–854 °C. COH fluids stabilise graphite and orthopyroxene; the high Mg#-ratio of biotite and pyroxenes, and apatite Cl < 2 a.p.f.u., indicate the importance of fluids during metamorphism. Stable isotopic δ 13 C graphite in the graphite schist is −38 to −17‰; δ 13 C calcite of marbles +3‰ to +10‰. Samples with both graphite and calcite present give lighter values for δ 13 C calcite = −8.7‰ to −9.5‰ and heavier values for δ 13 C graphite = −11.5‰ to −8.9‰. δ 18 O calcite for marble shows lighter values, ranging from −15.4‰ to −7.5‰. We interpret the graphite origin as organic carbon accumulated in sediments, while isotopic exchange between graphite and calcite reflects metamorphic and hydrothermal re-equilibration. |
format |
Article in Journal/Newspaper |
author |
Ane K. Engvik Håvard Gautneb Pål Tore Mørkved Janja Knežević Solberg Muriel Erambert |
author_facet |
Ane K. Engvik Håvard Gautneb Pål Tore Mørkved Janja Knežević Solberg Muriel Erambert |
author_sort |
Ane K. Engvik |
title |
Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway) |
title_short |
Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway) |
title_full |
Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway) |
title_fullStr |
Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway) |
title_full_unstemmed |
Proterozoic Deep Carbon—Characterisation, Origin and the Role of Fluids during High-Grade Metamorphism of Graphite (Lofoten–Vesterålen Complex, Norway) |
title_sort |
proterozoic deep carbon—characterisation, origin and the role of fluids during high-grade metamorphism of graphite (lofoten–vesterålen complex, norway) |
publisher |
MDPI AG |
publishDate |
2023 |
url |
https://doi.org/10.3390/min13101279 https://doaj.org/article/de460379b168461b8abb4e17b6ccdef5 |
genre |
Lofoten Northern Norway Vesterålen |
genre_facet |
Lofoten Northern Norway Vesterålen |
op_source |
Minerals, Vol 13, Iss 1279, p 1279 (2023) |
op_relation |
https://www.mdpi.com/2075-163X/13/10/1279 https://doaj.org/toc/2075-163X doi:10.3390/min13101279 2075-163X https://doaj.org/article/de460379b168461b8abb4e17b6ccdef5 |
op_doi |
https://doi.org/10.3390/min13101279 |
container_title |
Minerals |
container_volume |
13 |
container_issue |
10 |
container_start_page |
1279 |
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1782336508926099456 |