Carbon in mineralized ultramafic intrusions, caledonides, northern Britain

Parnell, J., Armstrong, J., Brolly, C., Boyce, A.J. and Heptinstall, E. (2020) Carbon in mineralized ultramafic intrusions, caledonides, northern Britain. Lithos, 374-5, 105711. (doi: 10.1016/j.lithos.2020.105711)

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Abstract

Graphite in Ordovician ultramafic intrusions through Neoproterozoic country rocks in West Aberdeenshire, NE Scotland attests to the mobility of carbon into subduction-related magmas. Pelites in the country rock contain up to 5% organic carbon, and are consequently also sulphide-rich. This occurrence is one of many examples of graphite in ultramafic intrusions. The sedimentary origin of the graphite carbon is indicated by carbon isotope compositions (mean − 19.7‰) in the same range as in the country rocks (mean − 21.6‰). The graphite is spatially and temporally associated with nickel-bearing sulphides, whose precipitation was strongly influenced by incorporation of the carbonaceous, sulphidic country rocks into the intrusions. Raman spectra for graphite in the intrusions show it is fully ordered, deposited from fluid in the magma. Preferential intrusion into pelitic country rocks facilitated the ready assimilation of carbon. In this case reworking of carbon from the crust into intrusions occurred 200 million years after sedimentation, a much longer timescale than most cycling of carbon in subduction zones.

Item Type:Articles
Additional Information:This work was partly supported by NERC grant NE/M010953/1.
Status:Published
Refereed:Yes
Glasgow Author(s) Enlighten ID:Boyce, Professor Adrian
Authors: Parnell, J., Armstrong, J., Brolly, C., Boyce, A.J., and Heptinstall, E.
College/School:College of Science and Engineering > Scottish Universities Environmental Research Centre
Journal Name:Lithos
Publisher:Elsevier
ISSN:0024-4937
ISSN (Online):1872-6143
Published Online:31 July 2020
Copyright Holders:Copyright © 2020 The Authors
First Published:First published in Lithos 374-5:105711
Publisher Policy:Reproduced under a Creative Commons licence

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