Sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on Rum and the wider North Atlantic Igneous Province
Ni–Cu–PGE (platinum group element) sulphide mineralization is commonly found in magmatic conduit systems. In many cases the trigger for formation of an immiscible sulphide liquid involves assimilation of S-bearing crustal rocks. Conceptually, the fluid dynamics of sulphide liquid droplets within suc...
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Oxford University Press (OUP)
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Online Access: | https://academic.oup.com/petrology/article/57/2/383/2453062/Sulphide-Sinking-in-Magma-Conduits-Evidence-from http://hdl.handle.net/2381/36905 https://doi.org/10.1093/petrology/egw010 |
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ftleicester:oai:lra.le.ac.uk:2381/36905 2023-05-15T16:03:57+02:00 Sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on Rum and the wider North Atlantic Igneous Province Hughes, Hannah S. R. McDonald, Iain Boyce, Adrian J. Holwell, David A. Kerr, Andrew C. 2016-02-26T10:59:03Z https://academic.oup.com/petrology/article/57/2/383/2453062/Sulphide-Sinking-in-Magma-Conduits-Evidence-from http://hdl.handle.net/2381/36905 https://doi.org/10.1093/petrology/egw010 en eng Oxford University Press (OUP) Journal of Petrology, 2016, 57 (2), 383-416. 0022-3530 https://academic.oup.com/petrology/article/57/2/383/2453062/Sulphide-Sinking-in-Magma-Conduits-Evidence-from http://hdl.handle.net/2381/36905 doi:10.1093/petrology/egw010 1460-2415 © The Author 2016. Published by Oxford University Press. This is an Open Access article distributed under the terms of the Creative Commons Attribution License ( http://creativecommons.org/licenses/by/4.0/ ), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. CC-BY Journal Article Article 2016 ftleicester https://doi.org/10.1093/petrology/egw010 2019-03-22T20:21:31Z Ni–Cu–PGE (platinum group element) sulphide mineralization is commonly found in magmatic conduit systems. In many cases the trigger for formation of an immiscible sulphide liquid involves assimilation of S-bearing crustal rocks. Conceptually, the fluid dynamics of sulphide liquid droplets within such conduits is essentially a balance between gravitational sinking and upwards entrainment. Thus, crustal contamination signatures may be present in sulphides preserved both up- and down-flow from the point of interaction with the contaminant. We examine a suite of ultramafic volcanic plugs on the Isle of Rum, Scotland, to decipher controls on sulphide accumulation in near-surface magma conduits intruded into a variable sedimentary stratigraphy. The whole-rock compositions of the plugs broadly overlap with the compositions of ultramafic units within the Rum Layered Complex, although subtle differences between each plug highlight their individuality. Interstitial base metal sulphide minerals occur in all ultramafic plugs on Rum. Sulphide minerals have magmatic δ 34 S (ranging from –1·3 to +2·1‰) and S/Se ratios (mean = 2299), and demonstrate that the conduit magmas were already S-saturated. However, two plugs in NW Rum contain substantially coarser (sometimes net-textured) sulphides with unusually light δ 34 S (–14·7 to +0·3‰) and elevated S/Se ratios (mean = 4457), not represented by the immediate host-rocks. Based on the Hebrides Basin sedimentary stratigraphy, it is likely that the volcanic con duits would have intruded through a package of Jurassic mudrocks with characteristically light δ 34 S (–33·8 to –14·7‰). We propose that a secondary crustal S contamination event took place at a level above that currently exposed, and that these sulphides sank back to their present position. Modelling suggests that upon the cessation of active magma transport, sulphide liquids could have sunk back through the conduit over a distance of several hundreds of metres, over a period of a few days. This sulphide ‘withdrawal’ process may be observed in other vertical or steeply inclined magma conduits globally; for example, in the macrodykes of East Greenland. Sulphide liquid sinking within a non-active conduit or during magma ‘suck-back’ may help to explain crustal S-isotopic compositions in magma conduits that appear to lack appropriate lithologies to support this contamination, either locally or deeper in the system. Peer-reviewed Publisher Version Article in Journal/Newspaper East Greenland Greenland North Atlantic University of Leicester: Leicester Research Archive (LRA) Greenland Journal of Petrology 57 2 383 416 |
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Open Polar |
collection |
University of Leicester: Leicester Research Archive (LRA) |
op_collection_id |
ftleicester |
language |
English |
description |
Ni–Cu–PGE (platinum group element) sulphide mineralization is commonly found in magmatic conduit systems. In many cases the trigger for formation of an immiscible sulphide liquid involves assimilation of S-bearing crustal rocks. Conceptually, the fluid dynamics of sulphide liquid droplets within such conduits is essentially a balance between gravitational sinking and upwards entrainment. Thus, crustal contamination signatures may be present in sulphides preserved both up- and down-flow from the point of interaction with the contaminant. We examine a suite of ultramafic volcanic plugs on the Isle of Rum, Scotland, to decipher controls on sulphide accumulation in near-surface magma conduits intruded into a variable sedimentary stratigraphy. The whole-rock compositions of the plugs broadly overlap with the compositions of ultramafic units within the Rum Layered Complex, although subtle differences between each plug highlight their individuality. Interstitial base metal sulphide minerals occur in all ultramafic plugs on Rum. Sulphide minerals have magmatic δ 34 S (ranging from –1·3 to +2·1‰) and S/Se ratios (mean = 2299), and demonstrate that the conduit magmas were already S-saturated. However, two plugs in NW Rum contain substantially coarser (sometimes net-textured) sulphides with unusually light δ 34 S (–14·7 to +0·3‰) and elevated S/Se ratios (mean = 4457), not represented by the immediate host-rocks. Based on the Hebrides Basin sedimentary stratigraphy, it is likely that the volcanic con duits would have intruded through a package of Jurassic mudrocks with characteristically light δ 34 S (–33·8 to –14·7‰). We propose that a secondary crustal S contamination event took place at a level above that currently exposed, and that these sulphides sank back to their present position. Modelling suggests that upon the cessation of active magma transport, sulphide liquids could have sunk back through the conduit over a distance of several hundreds of metres, over a period of a few days. This sulphide ‘withdrawal’ process may be observed in other vertical or steeply inclined magma conduits globally; for example, in the macrodykes of East Greenland. Sulphide liquid sinking within a non-active conduit or during magma ‘suck-back’ may help to explain crustal S-isotopic compositions in magma conduits that appear to lack appropriate lithologies to support this contamination, either locally or deeper in the system. Peer-reviewed Publisher Version |
format |
Article in Journal/Newspaper |
author |
Hughes, Hannah S. R. McDonald, Iain Boyce, Adrian J. Holwell, David A. Kerr, Andrew C. |
spellingShingle |
Hughes, Hannah S. R. McDonald, Iain Boyce, Adrian J. Holwell, David A. Kerr, Andrew C. Sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on Rum and the wider North Atlantic Igneous Province |
author_facet |
Hughes, Hannah S. R. McDonald, Iain Boyce, Adrian J. Holwell, David A. Kerr, Andrew C. |
author_sort |
Hughes, Hannah S. R. |
title |
Sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on Rum and the wider North Atlantic Igneous Province |
title_short |
Sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on Rum and the wider North Atlantic Igneous Province |
title_full |
Sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on Rum and the wider North Atlantic Igneous Province |
title_fullStr |
Sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on Rum and the wider North Atlantic Igneous Province |
title_full_unstemmed |
Sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on Rum and the wider North Atlantic Igneous Province |
title_sort |
sulphide sinking in magma conduits: evidence from mafic-ultramafic plugs on rum and the wider north atlantic igneous province |
publisher |
Oxford University Press (OUP) |
publishDate |
2016 |
url |
https://academic.oup.com/petrology/article/57/2/383/2453062/Sulphide-Sinking-in-Magma-Conduits-Evidence-from http://hdl.handle.net/2381/36905 https://doi.org/10.1093/petrology/egw010 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
East Greenland Greenland North Atlantic |
genre_facet |
East Greenland Greenland North Atlantic |
op_relation |
Journal of Petrology, 2016, 57 (2), 383-416. 0022-3530 https://academic.oup.com/petrology/article/57/2/383/2453062/Sulphide-Sinking-in-Magma-Conduits-Evidence-from http://hdl.handle.net/2381/36905 doi:10.1093/petrology/egw010 1460-2415 |
op_rights |
© The Author 2016. Published by Oxford University Press. This is an Open Access article distributed under the terms of the Creative Commons Attribution License ( http://creativecommons.org/licenses/by/4.0/ ), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1093/petrology/egw010 |
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Journal of Petrology |
container_volume |
57 |
container_issue |
2 |
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383 |
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416 |
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1766399649139130368 |