Crystal Storage and Transfer in Basaltic Systems: the Skuggafjoll Eruption, Iceland
Magma mixing and crystal mush disaggregation are important processes in basaltic magma reservoirs. We carried out a detailed petrological and geochemical study on a highly plagioclase-phyric eruption within the Eastern Volcanic Zone of Iceland—the Skuggafjöll eruption—to investigate crystal storage...
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fthighwire:oai:open-archive.highwire.org:petrology:55/12/2311 2023-05-15T16:48:44+02:00 Crystal Storage and Transfer in Basaltic Systems: the Skuggafjoll Eruption, Iceland Neave, David A. Maclennan, John Hartley, Margaret E. Edmonds, Marie Thordarson, Thorvaldur 2014-12-01 00:00:00.0 text/html http://petrology.oxfordjournals.org/cgi/content/short/55/12/2311 https://doi.org/10.1093/petrology/egu058 en eng Oxford University Press http://petrology.oxfordjournals.org/cgi/content/short/55/12/2311 http://dx.doi.org/10.1093/petrology/egu058 Copyright (C) 2014, Oxford University Press Original Papers TEXT 2014 fthighwire https://doi.org/10.1093/petrology/egu058 2015-02-28T19:09:23Z Magma mixing and crystal mush disaggregation are important processes in basaltic magma reservoirs. We carried out a detailed petrological and geochemical study on a highly plagioclase-phyric eruption within the Eastern Volcanic Zone of Iceland—the Skuggafjöll eruption—to investigate crystal storage and transport processes within a single magmatic system. Crystal content and phase proportions vary between samples: the least phyric samples have phase proportions similar to the low-pressure, three-phase gabbro eutectic (plg:cpx:ol ∼ 11:6:3), whereas highly phyric samples are strongly enriched in plagioclase (plg:cpx:ol ∼ 8:1:1). Statistically significant geochemical variability in 28 whole-rock samples collected across the eruption can be accounted for by variable accumulation of a troctolitic assemblage containing plagioclase and olivine in an approximately 9:1 ratio. Two macrocryst assemblages are defined using compositional and textural information recorded in QEMSCAN® images: a primitive assemblage of high-anorthite plagioclase (An >83 ) and high-forsterite olivine (Fo >84 ), and an evolved assemblage of low-anorthite plagioclase (An <79 ), low-forsterite olivine (Fo <82 ) and clinopyroxene (Mg# ∼ 82). Plagioclase and olivine have strongly bimodal composition distributions whereas the composition distribution of clinopyroxene is unimodal. The mean trace element composition of melt inclusions hosted within high-forsterite olivine and high-anorthite plagioclase macrocrysts is the same (mean Ce/Y ∼ 0·47–0·48), confirming that both primitive macrocryst phases crystallized from the same distribution of melts. Clinopyroxene macrocrysts and matrix glasses are in Ce/Yb equilibrium with each other, indicating that the evolved assemblage crystallized from melts with a more incompatible trace element-enriched composition (mean Ce/Y ∼ 0·65–71) than the primitive assemblage. Variability in whole-rock, macrocryst and melt inclusion compositions suggests that the Skuggafjöll magma experienced two stages of ... Text Iceland HighWire Press (Stanford University) Skuggafjöll ENVELOPE(-18.722,-18.722,63.977,63.977) Journal of Petrology 55 12 2311 2346 |
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HighWire Press (Stanford University) |
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English |
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Original Papers |
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Original Papers Neave, David A. Maclennan, John Hartley, Margaret E. Edmonds, Marie Thordarson, Thorvaldur Crystal Storage and Transfer in Basaltic Systems: the Skuggafjoll Eruption, Iceland |
topic_facet |
Original Papers |
description |
Magma mixing and crystal mush disaggregation are important processes in basaltic magma reservoirs. We carried out a detailed petrological and geochemical study on a highly plagioclase-phyric eruption within the Eastern Volcanic Zone of Iceland—the Skuggafjöll eruption—to investigate crystal storage and transport processes within a single magmatic system. Crystal content and phase proportions vary between samples: the least phyric samples have phase proportions similar to the low-pressure, three-phase gabbro eutectic (plg:cpx:ol ∼ 11:6:3), whereas highly phyric samples are strongly enriched in plagioclase (plg:cpx:ol ∼ 8:1:1). Statistically significant geochemical variability in 28 whole-rock samples collected across the eruption can be accounted for by variable accumulation of a troctolitic assemblage containing plagioclase and olivine in an approximately 9:1 ratio. Two macrocryst assemblages are defined using compositional and textural information recorded in QEMSCAN® images: a primitive assemblage of high-anorthite plagioclase (An >83 ) and high-forsterite olivine (Fo >84 ), and an evolved assemblage of low-anorthite plagioclase (An <79 ), low-forsterite olivine (Fo <82 ) and clinopyroxene (Mg# ∼ 82). Plagioclase and olivine have strongly bimodal composition distributions whereas the composition distribution of clinopyroxene is unimodal. The mean trace element composition of melt inclusions hosted within high-forsterite olivine and high-anorthite plagioclase macrocrysts is the same (mean Ce/Y ∼ 0·47–0·48), confirming that both primitive macrocryst phases crystallized from the same distribution of melts. Clinopyroxene macrocrysts and matrix glasses are in Ce/Yb equilibrium with each other, indicating that the evolved assemblage crystallized from melts with a more incompatible trace element-enriched composition (mean Ce/Y ∼ 0·65–71) than the primitive assemblage. Variability in whole-rock, macrocryst and melt inclusion compositions suggests that the Skuggafjöll magma experienced two stages of ... |
format |
Text |
author |
Neave, David A. Maclennan, John Hartley, Margaret E. Edmonds, Marie Thordarson, Thorvaldur |
author_facet |
Neave, David A. Maclennan, John Hartley, Margaret E. Edmonds, Marie Thordarson, Thorvaldur |
author_sort |
Neave, David A. |
title |
Crystal Storage and Transfer in Basaltic Systems: the Skuggafjoll Eruption, Iceland |
title_short |
Crystal Storage and Transfer in Basaltic Systems: the Skuggafjoll Eruption, Iceland |
title_full |
Crystal Storage and Transfer in Basaltic Systems: the Skuggafjoll Eruption, Iceland |
title_fullStr |
Crystal Storage and Transfer in Basaltic Systems: the Skuggafjoll Eruption, Iceland |
title_full_unstemmed |
Crystal Storage and Transfer in Basaltic Systems: the Skuggafjoll Eruption, Iceland |
title_sort |
crystal storage and transfer in basaltic systems: the skuggafjoll eruption, iceland |
publisher |
Oxford University Press |
publishDate |
2014 |
url |
http://petrology.oxfordjournals.org/cgi/content/short/55/12/2311 https://doi.org/10.1093/petrology/egu058 |
long_lat |
ENVELOPE(-18.722,-18.722,63.977,63.977) |
geographic |
Skuggafjöll |
geographic_facet |
Skuggafjöll |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
http://petrology.oxfordjournals.org/cgi/content/short/55/12/2311 http://dx.doi.org/10.1093/petrology/egu058 |
op_rights |
Copyright (C) 2014, Oxford University Press |
op_doi |
https://doi.org/10.1093/petrology/egu058 |
container_title |
Journal of Petrology |
container_volume |
55 |
container_issue |
12 |
container_start_page |
2311 |
op_container_end_page |
2346 |
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1766038810201686016 |