Experimental study of the influence of water on melting and phase assemblages in the upper mantle

David H. Green, William O. Hibberson, Anja Rosenthal, I. Kovács, Gregory M. Yaxley, Trevorj Falloon, Frank Brink

Research output: Article

70 Citations (Scopus)

Abstract

The role of water in the uppermost mantle has been explored to 6GPa (~200 km) by a novel experimental approach in which the silicate melting solidus, the stability of hydrous phases and the H2O contents in nominally anhydrous minerals (NAMs) were determined. The composition studied is a fertile lherzolite modelled as a source for mid-ocean ridge basalts (MORB). The use of crushed olivine as traps for melt or fluid inclusions allows a distinction to be made between quenched hydrous silicate melt and quench material from water-rich vapour phase.The vapor-saturated solidus (waterrich vapor) of fertile lherzolite increases in temperature (T) from a minimum of 9708C at 1·5GPa (~50 km) to 13758C at 6GPa. The Ca-rich amphibole pargasite is stable to the vapour-saturated solidus to 3 GPa (~100 km). Based on normative components, at 2·5 GPa the near-solidus melt (1-2%) in mantle with very low H2O content is transitional between sodic-dolomitic carbonatite and olivine melilitite.With higher melt fraction (~5%) at higher Tor higher H2O content it is olivine-rich basanite. Both immediately below and above the solidus, the H2O content in residual lherzolite is ~200 ppm retained in NAMs at 2·5 and 4GPa.The experimentally determined vapour-saturated solidus corrects recent numerical models of melting of lherzolite+H2O based on inferred high solubilities of H2O in NAMs and accounts for a discrepant experimental determination of the vapour-saturated solidus in which very high water/rock ratios were used. At 2·5±0·1GPa, the water content of experimental charges was varied from 0·05 to 14·5wt %. Below the solidus and with increasing water content from 0·05 to 2·9 wt %, pargasite decreases in K2O and Na2O content and is absent in experiments with 7·25 and 14·5wt % H2O. Also with increasing water content from 0·05 to 14·5wt % H2O, the Na2O content of clinopyroxene decreases from 1·6 wt % to below the limit of detection (0·2 wt %). The destabilization of pargasite and change of clinopyroxene composition at 2·5GPa and 10008C are attributed to the leaching role (Na2O and c particularly) of the water-rich vapour at high water/rock ratios. The hydrous mineral pargasite is the major site of H2O storage in fertile uppermost mantle lherzolite but pargasite is unstable at pressures (P) > 3GPa (~100 km depth), causing a sharp drop in the water storage capacity of the upper mantle from > 2000 to ~200 ppm. For small H2O contents (<2000 ppm approximately), the temperature of the vapourundersaturated solidus of fertile upper mantle lherzolite decreases sharply with increasing P at ~90 km depth.The negative dT/dP for the vapour-undersaturated solidus has important rheological and geodynamic consequences. In oceanic intraplate settings, the geotherm passes from subsolidus pargasite-bearing lherzolite to garnet lherzolite with incipient melting, creating the rheological boundary at ~90 km depth, between lithosphere and asthenosphere.The asthenosphere becomes geochemically zoned with the 'enriched' intraplate basalt source (>500 ppm H2O) overlying the 'depleted' MORB source (~200 ppm H2O) in the deeper asthenosphere.Water also plays a significant role at convergent margins, where hydrous silicate melting in the mantle wedge is initiated at the vapour-saturated solidus. Melting of lherzolite at or near the vapour-saturated solidus does not fully dehydrate residual lherzolite or harzburgite. Residual lithosphere returned to the upper mantle may carry ~100-200 ppm H2O. At 6 GPa the low K/Na model mantle composition (MORBsource mantle) with > 200 ppm H2O has normal rather than supercritical melting behaviour with the solidus at 1375°C, which is ~350°C below the C+H-free solidus.

Original languageEnglish
Pages (from-to)2067-2096
Number of pages30
JournalJournal of Petrology
Volume55
Issue number10
DOIs
Publication statusPublished - okt. 1 2014

Fingerprint

solidus
lherzolite
pargasite
upper mantle
Earth mantle
Melting
experimental study
melting
Vapors
mantle
Water
water
Silicates
vapors
Minerals
olivine
water content
Water content
mid-ocean ridge basalt
clinopyroxene

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

Cite this

Green, D. H., Hibberson, W. O., Rosenthal, A., Kovács, I., Yaxley, G. M., Falloon, T., & Brink, F. (2014). Experimental study of the influence of water on melting and phase assemblages in the upper mantle. Journal of Petrology, 55(10), 2067-2096. https://doi.org/10.1093/petrology/egu050

Experimental study of the influence of water on melting and phase assemblages in the upper mantle. / Green, David H.; Hibberson, William O.; Rosenthal, Anja; Kovács, I.; Yaxley, Gregory M.; Falloon, Trevorj; Brink, Frank.

In: Journal of Petrology, Vol. 55, No. 10, 01.10.2014, p. 2067-2096.

Research output: Article

Green, DH, Hibberson, WO, Rosenthal, A, Kovács, I, Yaxley, GM, Falloon, T & Brink, F 2014, 'Experimental study of the influence of water on melting and phase assemblages in the upper mantle', Journal of Petrology, vol. 55, no. 10, pp. 2067-2096. https://doi.org/10.1093/petrology/egu050
Green, David H. ; Hibberson, William O. ; Rosenthal, Anja ; Kovács, I. ; Yaxley, Gregory M. ; Falloon, Trevorj ; Brink, Frank. / Experimental study of the influence of water on melting and phase assemblages in the upper mantle. In: Journal of Petrology. 2014 ; Vol. 55, No. 10. pp. 2067-2096.
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abstract = "The role of water in the uppermost mantle has been explored to 6GPa (~200 km) by a novel experimental approach in which the silicate melting solidus, the stability of hydrous phases and the H2O contents in nominally anhydrous minerals (NAMs) were determined. The composition studied is a fertile lherzolite modelled as a source for mid-ocean ridge basalts (MORB). The use of crushed olivine as traps for melt or fluid inclusions allows a distinction to be made between quenched hydrous silicate melt and quench material from water-rich vapour phase.The vapor-saturated solidus (waterrich vapor) of fertile lherzolite increases in temperature (T) from a minimum of 9708C at 1·5GPa (~50 km) to 13758C at 6GPa. The Ca-rich amphibole pargasite is stable to the vapour-saturated solidus to 3 GPa (~100 km). Based on normative components, at 2·5 GPa the near-solidus melt (1-2{\%}) in mantle with very low H2O content is transitional between sodic-dolomitic carbonatite and olivine melilitite.With higher melt fraction (~5{\%}) at higher Tor higher H2O content it is olivine-rich basanite. Both immediately below and above the solidus, the H2O content in residual lherzolite is ~200 ppm retained in NAMs at 2·5 and 4GPa.The experimentally determined vapour-saturated solidus corrects recent numerical models of melting of lherzolite+H2O based on inferred high solubilities of H2O in NAMs and accounts for a discrepant experimental determination of the vapour-saturated solidus in which very high water/rock ratios were used. At 2·5±0·1GPa, the water content of experimental charges was varied from 0·05 to 14·5wt {\%}. Below the solidus and with increasing water content from 0·05 to 2·9 wt {\%}, pargasite decreases in K2O and Na2O content and is absent in experiments with 7·25 and 14·5wt {\%} H2O. Also with increasing water content from 0·05 to 14·5wt {\%} H2O, the Na2O content of clinopyroxene decreases from 1·6 wt {\%} to below the limit of detection (0·2 wt {\%}). The destabilization of pargasite and change of clinopyroxene composition at 2·5GPa and 10008C are attributed to the leaching role (Na2O and c particularly) of the water-rich vapour at high water/rock ratios. The hydrous mineral pargasite is the major site of H2O storage in fertile uppermost mantle lherzolite but pargasite is unstable at pressures (P) > 3GPa (~100 km depth), causing a sharp drop in the water storage capacity of the upper mantle from > 2000 to ~200 ppm. For small H2O contents (<2000 ppm approximately), the temperature of the vapourundersaturated solidus of fertile upper mantle lherzolite decreases sharply with increasing P at ~90 km depth.The negative dT/dP for the vapour-undersaturated solidus has important rheological and geodynamic consequences. In oceanic intraplate settings, the geotherm passes from subsolidus pargasite-bearing lherzolite to garnet lherzolite with incipient melting, creating the rheological boundary at ~90 km depth, between lithosphere and asthenosphere.The asthenosphere becomes geochemically zoned with the 'enriched' intraplate basalt source (>500 ppm H2O) overlying the 'depleted' MORB source (~200 ppm H2O) in the deeper asthenosphere.Water also plays a significant role at convergent margins, where hydrous silicate melting in the mantle wedge is initiated at the vapour-saturated solidus. Melting of lherzolite at or near the vapour-saturated solidus does not fully dehydrate residual lherzolite or harzburgite. Residual lithosphere returned to the upper mantle may carry ~100-200 ppm H2O. At 6 GPa the low K/Na model mantle composition (MORBsource mantle) with > 200 ppm H2O has normal rather than supercritical melting behaviour with the solidus at 1375°C, which is ~350°C below the C+H-free solidus.",
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T1 - Experimental study of the influence of water on melting and phase assemblages in the upper mantle

AU - Green, David H.

AU - Hibberson, William O.

AU - Rosenthal, Anja

AU - Kovács, I.

AU - Yaxley, Gregory M.

AU - Falloon, Trevorj

AU - Brink, Frank

PY - 2014/10/1

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N2 - The role of water in the uppermost mantle has been explored to 6GPa (~200 km) by a novel experimental approach in which the silicate melting solidus, the stability of hydrous phases and the H2O contents in nominally anhydrous minerals (NAMs) were determined. The composition studied is a fertile lherzolite modelled as a source for mid-ocean ridge basalts (MORB). The use of crushed olivine as traps for melt or fluid inclusions allows a distinction to be made between quenched hydrous silicate melt and quench material from water-rich vapour phase.The vapor-saturated solidus (waterrich vapor) of fertile lherzolite increases in temperature (T) from a minimum of 9708C at 1·5GPa (~50 km) to 13758C at 6GPa. The Ca-rich amphibole pargasite is stable to the vapour-saturated solidus to 3 GPa (~100 km). Based on normative components, at 2·5 GPa the near-solidus melt (1-2%) in mantle with very low H2O content is transitional between sodic-dolomitic carbonatite and olivine melilitite.With higher melt fraction (~5%) at higher Tor higher H2O content it is olivine-rich basanite. Both immediately below and above the solidus, the H2O content in residual lherzolite is ~200 ppm retained in NAMs at 2·5 and 4GPa.The experimentally determined vapour-saturated solidus corrects recent numerical models of melting of lherzolite+H2O based on inferred high solubilities of H2O in NAMs and accounts for a discrepant experimental determination of the vapour-saturated solidus in which very high water/rock ratios were used. At 2·5±0·1GPa, the water content of experimental charges was varied from 0·05 to 14·5wt %. Below the solidus and with increasing water content from 0·05 to 2·9 wt %, pargasite decreases in K2O and Na2O content and is absent in experiments with 7·25 and 14·5wt % H2O. Also with increasing water content from 0·05 to 14·5wt % H2O, the Na2O content of clinopyroxene decreases from 1·6 wt % to below the limit of detection (0·2 wt %). The destabilization of pargasite and change of clinopyroxene composition at 2·5GPa and 10008C are attributed to the leaching role (Na2O and c particularly) of the water-rich vapour at high water/rock ratios. The hydrous mineral pargasite is the major site of H2O storage in fertile uppermost mantle lherzolite but pargasite is unstable at pressures (P) > 3GPa (~100 km depth), causing a sharp drop in the water storage capacity of the upper mantle from > 2000 to ~200 ppm. For small H2O contents (<2000 ppm approximately), the temperature of the vapourundersaturated solidus of fertile upper mantle lherzolite decreases sharply with increasing P at ~90 km depth.The negative dT/dP for the vapour-undersaturated solidus has important rheological and geodynamic consequences. In oceanic intraplate settings, the geotherm passes from subsolidus pargasite-bearing lherzolite to garnet lherzolite with incipient melting, creating the rheological boundary at ~90 km depth, between lithosphere and asthenosphere.The asthenosphere becomes geochemically zoned with the 'enriched' intraplate basalt source (>500 ppm H2O) overlying the 'depleted' MORB source (~200 ppm H2O) in the deeper asthenosphere.Water also plays a significant role at convergent margins, where hydrous silicate melting in the mantle wedge is initiated at the vapour-saturated solidus. Melting of lherzolite at or near the vapour-saturated solidus does not fully dehydrate residual lherzolite or harzburgite. Residual lithosphere returned to the upper mantle may carry ~100-200 ppm H2O. At 6 GPa the low K/Na model mantle composition (MORBsource mantle) with > 200 ppm H2O has normal rather than supercritical melting behaviour with the solidus at 1375°C, which is ~350°C below the C+H-free solidus.

AB - The role of water in the uppermost mantle has been explored to 6GPa (~200 km) by a novel experimental approach in which the silicate melting solidus, the stability of hydrous phases and the H2O contents in nominally anhydrous minerals (NAMs) were determined. The composition studied is a fertile lherzolite modelled as a source for mid-ocean ridge basalts (MORB). The use of crushed olivine as traps for melt or fluid inclusions allows a distinction to be made between quenched hydrous silicate melt and quench material from water-rich vapour phase.The vapor-saturated solidus (waterrich vapor) of fertile lherzolite increases in temperature (T) from a minimum of 9708C at 1·5GPa (~50 km) to 13758C at 6GPa. The Ca-rich amphibole pargasite is stable to the vapour-saturated solidus to 3 GPa (~100 km). Based on normative components, at 2·5 GPa the near-solidus melt (1-2%) in mantle with very low H2O content is transitional between sodic-dolomitic carbonatite and olivine melilitite.With higher melt fraction (~5%) at higher Tor higher H2O content it is olivine-rich basanite. Both immediately below and above the solidus, the H2O content in residual lherzolite is ~200 ppm retained in NAMs at 2·5 and 4GPa.The experimentally determined vapour-saturated solidus corrects recent numerical models of melting of lherzolite+H2O based on inferred high solubilities of H2O in NAMs and accounts for a discrepant experimental determination of the vapour-saturated solidus in which very high water/rock ratios were used. At 2·5±0·1GPa, the water content of experimental charges was varied from 0·05 to 14·5wt %. Below the solidus and with increasing water content from 0·05 to 2·9 wt %, pargasite decreases in K2O and Na2O content and is absent in experiments with 7·25 and 14·5wt % H2O. Also with increasing water content from 0·05 to 14·5wt % H2O, the Na2O content of clinopyroxene decreases from 1·6 wt % to below the limit of detection (0·2 wt %). The destabilization of pargasite and change of clinopyroxene composition at 2·5GPa and 10008C are attributed to the leaching role (Na2O and c particularly) of the water-rich vapour at high water/rock ratios. The hydrous mineral pargasite is the major site of H2O storage in fertile uppermost mantle lherzolite but pargasite is unstable at pressures (P) > 3GPa (~100 km depth), causing a sharp drop in the water storage capacity of the upper mantle from > 2000 to ~200 ppm. For small H2O contents (<2000 ppm approximately), the temperature of the vapourundersaturated solidus of fertile upper mantle lherzolite decreases sharply with increasing P at ~90 km depth.The negative dT/dP for the vapour-undersaturated solidus has important rheological and geodynamic consequences. In oceanic intraplate settings, the geotherm passes from subsolidus pargasite-bearing lherzolite to garnet lherzolite with incipient melting, creating the rheological boundary at ~90 km depth, between lithosphere and asthenosphere.The asthenosphere becomes geochemically zoned with the 'enriched' intraplate basalt source (>500 ppm H2O) overlying the 'depleted' MORB source (~200 ppm H2O) in the deeper asthenosphere.Water also plays a significant role at convergent margins, where hydrous silicate melting in the mantle wedge is initiated at the vapour-saturated solidus. Melting of lherzolite at or near the vapour-saturated solidus does not fully dehydrate residual lherzolite or harzburgite. Residual lithosphere returned to the upper mantle may carry ~100-200 ppm H2O. At 6 GPa the low K/Na model mantle composition (MORBsource mantle) with > 200 ppm H2O has normal rather than supercritical melting behaviour with the solidus at 1375°C, which is ~350°C below the C+H-free solidus.

KW - Asthenosphere

KW - Experimental petrology

KW - Hydrous mineral phases pargasite and phlogopite

KW - Lithosphere

KW - Nominally anhydrous minerals

KW - Upper mantle melting

KW - Water in the upper mantle

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