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<title>UTas ePrints - Peridotite Melting at 1 GPa: Reversal Experiments on Partial Melt Compositions Produced by Peridotite-Basalt Sandwich Experiments</title>
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<meta content="Falloon, T.J." name="eprints.creators_name" />
<meta content="Danyushevsky, L.V." name="eprints.creators_name" />
<meta content="Green, D.H." name="eprints.creators_name" />
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<meta content="2007-02-14" name="eprints.datestamp" />
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<meta content="mantle melting; sandwich experiments; reversal experiments; anhydrous peridotite melting; thermocouple oxidation; olivine geothermometry" name="eprints.keywords" />
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<meta content="One of the goals of igneous petrology is to use the subtle and more obvious differences in the geochemistry of primitive basalts to place constraints on mantle composition, melting conditions and dynamics of mantle upwelling and melt extraction. For this goal to be achieved, our first-order understanding of mantle melting must be refined by high-quality, systematic data on correlated melt and residual phase compositions under known pressures and temperatures. Discrepancies in earlier data on melt compositions from a fertile mantle composition [MORB (mid-ocean ridge basalt) Pyrolite mg-number 87] and refractory lherzolite (Tinaquillo Lherzolite mg-number 90) are resolved here. Errors in earlier data resulted from drift of W/Re thermocouples at 1 GPa and access of water, lowering liquidus temperatures by 30-80 degrees C. We demonstrate the suitability of the 'sandwich' technique for determining the compositions of multiphase-saturated liquids in lherzolite, provided fine-grained sintered oxide mixes are used as the peridotite starting materials, and the changes in bulk composition are considered. Compositions of liquids in equilibrium with lherzolitic to harzburgitic residue at 1 GPa, 1300-1450degrees C in the two lherzolite compositions are reported. Melt compositions are olivine + hypersthene-normative (olivine tholeiites) with the more refractory composition producing a lower melt fraction (7-8% at 1300 degrees C) compared with the model MORB source (18-20% at 1300 degrees C)." name="eprints.abstract" />
<meta content="2001" name="eprints.date" />
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<meta content="Falloon, T.J. and Danyushevsky, L.V. and Green, D.H. (2001) Peridotite Melting at 1 GPa: Reversal Experiments on Partial Melt Compositions Produced by Peridotite-Basalt Sandwich Experiments. Journal of Petrology, 42 (12). pp. 2363-2390." name="eprints.citation" />
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<meta content="One of the goals of igneous petrology is to use the subtle and more obvious differences in the geochemistry of primitive basalts to place constraints on mantle composition, melting conditions and dynamics of mantle upwelling and melt extraction. For this goal to be achieved, our first-order understanding of mantle melting must be refined by high-quality, systematic data on correlated melt and residual phase compositions under known pressures and temperatures. Discrepancies in earlier data on melt compositions from a fertile mantle composition [MORB (mid-ocean ridge basalt) Pyrolite mg-number 87] and refractory lherzolite (Tinaquillo Lherzolite mg-number 90) are resolved here. Errors in earlier data resulted from drift of W/Re thermocouples at 1 GPa and access of water, lowering liquidus temperatures by 30-80 degrees C. We demonstrate the suitability of the 'sandwich' technique for determining the compositions of multiphase-saturated liquids in lherzolite, provided fine-grained sintered oxide mixes are used as the peridotite starting materials, and the changes in bulk composition are considered. Compositions of liquids in equilibrium with lherzolitic to harzburgitic residue at 1 GPa, 1300-1450degrees C in the two lherzolite compositions are reported. Melt compositions are olivine + hypersthene-normative (olivine tholeiites) with the more refractory composition producing a lower melt fraction (7-8% at 1300 degrees C) compared with the model MORB source (18-20% at 1300 degrees C)." name="DC.description" />
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<h1 class="ep_tm_pagetitle">Peridotite Melting at 1 GPa: Reversal Experiments on Partial Melt Compositions Produced by Peridotite-Basalt Sandwich Experiments</h1>
<p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Falloon, T.J.</span> and <span class="person_name">Danyushevsky, L.V.</span> and <span class="person_name">Green, D.H.</span> (2001) <xhtml:em>Peridotite Melting at 1 GPa: Reversal Experiments on Partial Melt Compositions Produced by Peridotite-Basalt Sandwich Experiments.</xhtml:em> Journal of Petrology, 42 (12). pp. 2363-2390.</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a href="http://eprints.utas.edu.au/707/1/Falloon_et_al_2001.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/707/1/Falloon_et_al_2001.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />322Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input accept-charset="utf-8" value="719" name="docid" type="hidden" /><div class=""><input value="Request a copy" name="_action_null" class="ep_form_action_button" onclick="return EPJS_button_pushed( '_action_null' )" type="submit" /> </div></form></td></tr></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://petrology.oxfordjournals.org/">http://petrology.oxfordjournals.org/</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">One of the goals of igneous petrology is to use the subtle and more obvious differences in the geochemistry of primitive basalts to place constraints on mantle composition, melting conditions and dynamics of mantle upwelling and melt extraction. For this goal to be achieved, our first-order understanding of mantle melting must be refined by high-quality, systematic data on correlated melt and residual phase compositions under known pressures and temperatures. Discrepancies in earlier data on melt compositions from a fertile mantle composition [MORB (mid-ocean ridge basalt) Pyrolite mg-number 87] and refractory lherzolite (Tinaquillo Lherzolite mg-number 90) are resolved here. Errors in earlier data resulted from drift of W/Re thermocouples at 1 GPa and access of water, lowering liquidus temperatures by 30-80 degrees C. We demonstrate the suitability of the 'sandwich' technique for determining the compositions of multiphase-saturated liquids in lherzolite, provided fine-grained sintered oxide mixes are used as the peridotite starting materials, and the changes in bulk composition are considered. Compositions of liquids in equilibrium with lherzolitic to harzburgitic residue at 1 GPa, 1300-1450degrees C in the two lherzolite compositions are reported. Melt compositions are olivine + hypersthene-normative (olivine tholeiites) with the more refractory composition producing a lower melt fraction (7-8% at 1300 degrees C) compared with the model MORB source (18-20% at 1300 degrees C).</p></div><table style="margin-bottom: 1em" cellpadding="3" class="not_ep_block" border="0"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Article</td></tr><tr><th valign="top" class="ep_row">Additional Information:</th><td valign="top" class="ep_row">The definitive publisher-authenticated version is available online at: http://petrology.oxfordjournals.org/</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">mantle melting; sandwich experiments; reversal experiments; anhydrous peridotite melting; thermocouple oxidation; olivine geothermometry</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/260100.html">260000 Earth Sciences > 260100 Geology</a></td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">707</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">Mr Ruben Chan</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">14 Feb 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">09 Jan 2008 02:30</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=707;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&eprintid=707">item control page</a></p>
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