Mixed metamorphic and fluid graphite deposition in Palaeoproterozoic supracrustal rocks of the Lewisian Complex, NW Scotland

Graphite deposits may form alternatively by metamorphism of sedimentary rocks and from fluids. Both types occur in supracrustal successions within the Lewisian Complex of Northwest Scotland, and similarly in Palaeoproterozoic supracrustal rocks across the North Atlantic region in Canada, Greenland a...

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Veröffentlicht in:	Terra nova (Oxford, England) England), 2021-12, Vol.33 (6), p.541-550
Hauptverfasser:	Parnell, John, Brolly, Connor, Boyce, Adrian J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Analytical methods carbon Carbon isotopes Fluids Graphite Isotopes Lewisian marble Metamorphism Organic matter Palaeoproterozoic Raman spectroscopy Schists Scotland Sedimentary facies Sedimentary rocks Survival
Online-Zugang:	Volltext
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