Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island
The effects of source composition and source evolution during progressive partial melting on the chemistry of mantle-derived mid-ocean ridge basalt (MORB) melts were tested using a comprehensive geochemical and Sr-Nd-Pb isotopic dataset for fresh, magnesian basaltic glasses from the Miocene Macquari...
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ftunivtasecite:oai:ecite.utas.edu.au:24739 2023-05-15T17:09:55+02:00 Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island Kamenetsky, VS Maas, R 2002 https://doi.org/10.1093/petrology/43.10.1909 http://ecite.utas.edu.au/24739 en eng Oxford University Press http://dx.doi.org/10.1093/petrology/43.10.1909 Kamenetsky, VS and Maas, R, Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island, Journal of Petrology, 43, (10) pp. 1909-1922. ISSN 0022-3530 (2002) [Refereed Article] http://ecite.utas.edu.au/24739 Earth Sciences Geology Igneous and Metamorphic Petrology Refereed Article PeerReviewed 2002 ftunivtasecite https://doi.org/10.1093/petrology/43.10.1909 2019-12-13T21:06:00Z The effects of source composition and source evolution during progressive partial melting on the chemistry of mantle-derived mid-ocean ridge basalt (MORB) melts were tested using a comprehensive geochemical and Sr-Nd-Pb isotopic dataset for fresh, magnesian basaltic glasses from the Miocene Macquarie Island ophiolite, SW Pacific. These glasses: (1) exhibit clear parent-daughter relationships; (2) allow simple reconstruction of primary melt compositions; (3) show exceptional compositional diversity (e.g. K2O/TiO2 0.09-0.9; La/Yb 1.5-22; 206Pb/204Pb 18.70-19.52); (4) preserve changes in major element and isotope compositions, which are correlated with the degree of trace element enrichment (e.g. La/Sm). Conventional models for MORB genesis invoke melting of mantle that is heterogeneous on a small scale, followed by binary mixing of variably lithophile element-enriched melt batches. This type of model fails to explain the compositions of the Macquarie Island glasses, principally because incompatible element ratios (e.g. Nb/U, Sr/Nd) and Pb isotope ratios vary non-systematically with the degree of enrichment. We propose that individual melt batches are produced from instantaneous 'parental' mantle parageneses, which change continuously as melting and melt extraction proceeds. This concept of a 'dynamic source' combines the models of small-scale mantle heterogeneities and fractional melting. A dynamic source is an assemblage of locally equilibrated mantle solids and a related melt fraction. Common MORB magmas that integrate the characteristics of numerous melt batches therefore tend to conceal the chemical and isotopic identity of a dynamic source. This study shows that isotope ratios of poorly mixed MORB melts are a complex function of the dynamic source evolution, and that the range in isotope ratios within a single MORB suite does not necessarily require mixing of diverse components. Article in Journal/Newspaper Macquarie Island eCite UTAS (University of Tasmania) Pacific Journal of Petrology 43 10 1909 1922 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Geology Igneous and Metamorphic Petrology |
spellingShingle |
Earth Sciences Geology Igneous and Metamorphic Petrology Kamenetsky, VS Maas, R Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island |
topic_facet |
Earth Sciences Geology Igneous and Metamorphic Petrology |
description |
The effects of source composition and source evolution during progressive partial melting on the chemistry of mantle-derived mid-ocean ridge basalt (MORB) melts were tested using a comprehensive geochemical and Sr-Nd-Pb isotopic dataset for fresh, magnesian basaltic glasses from the Miocene Macquarie Island ophiolite, SW Pacific. These glasses: (1) exhibit clear parent-daughter relationships; (2) allow simple reconstruction of primary melt compositions; (3) show exceptional compositional diversity (e.g. K2O/TiO2 0.09-0.9; La/Yb 1.5-22; 206Pb/204Pb 18.70-19.52); (4) preserve changes in major element and isotope compositions, which are correlated with the degree of trace element enrichment (e.g. La/Sm). Conventional models for MORB genesis invoke melting of mantle that is heterogeneous on a small scale, followed by binary mixing of variably lithophile element-enriched melt batches. This type of model fails to explain the compositions of the Macquarie Island glasses, principally because incompatible element ratios (e.g. Nb/U, Sr/Nd) and Pb isotope ratios vary non-systematically with the degree of enrichment. We propose that individual melt batches are produced from instantaneous 'parental' mantle parageneses, which change continuously as melting and melt extraction proceeds. This concept of a 'dynamic source' combines the models of small-scale mantle heterogeneities and fractional melting. A dynamic source is an assemblage of locally equilibrated mantle solids and a related melt fraction. Common MORB magmas that integrate the characteristics of numerous melt batches therefore tend to conceal the chemical and isotopic identity of a dynamic source. This study shows that isotope ratios of poorly mixed MORB melts are a complex function of the dynamic source evolution, and that the range in isotope ratios within a single MORB suite does not necessarily require mixing of diverse components. |
format |
Article in Journal/Newspaper |
author |
Kamenetsky, VS Maas, R |
author_facet |
Kamenetsky, VS Maas, R |
author_sort |
Kamenetsky, VS |
title |
Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island |
title_short |
Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island |
title_full |
Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island |
title_fullStr |
Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island |
title_full_unstemmed |
Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island |
title_sort |
mantle-melt evolution (dynamic source) in the origin of a single morb suite: a perspective from magnesian glasses of macquarie island |
publisher |
Oxford University Press |
publishDate |
2002 |
url |
https://doi.org/10.1093/petrology/43.10.1909 http://ecite.utas.edu.au/24739 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Macquarie Island |
genre_facet |
Macquarie Island |
op_relation |
http://dx.doi.org/10.1093/petrology/43.10.1909 Kamenetsky, VS and Maas, R, Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island, Journal of Petrology, 43, (10) pp. 1909-1922. ISSN 0022-3530 (2002) [Refereed Article] http://ecite.utas.edu.au/24739 |
op_doi |
https://doi.org/10.1093/petrology/43.10.1909 |
container_title |
Journal of Petrology |
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43 |
container_issue |
10 |
container_start_page |
1909 |
op_container_end_page |
1922 |
_version_ |
1766066293582069760 |