Experimental alteration of monazite in granitic melt: Variable U–Th–Pb and REE mobility during melt-mediated coupled dissolution-precipitation

dc.contributor.authorVarga, J.
dc.contributor.authorRaimondo, T.
dc.contributor.authorDaczko, N.R.
dc.contributor.authorAdam, J.
dc.date.issued2020
dc.description.abstractMonazite U–Th–Pb geochronology of high-temperature and melt-bearing metamorphic rocks sometimes produces a continuum of concordant ages (‘smear’) without well-defined age populations. In combination with textural and geochemical criteria, these datasets are typically interpreted to infer either variable Pb-loss between two discrete events or protracted metamorphism lasting >50 Myr. We experimentally react monazite with granitic melt (0.7 GPa and 750 °C) to produce a range of complex monazite textures and age patterns similar to those found in natural high-temperature rock samples. Our observations show that within a short duration (≤24 h experiment time), variable REE, Y, Th, U and Pb mobility is achieved via coupled dissolution-precipitation in a melt-bearing system. An ultra-local interface melt is saturated in dissolved components, including the U–Th–Pb isotopic character of the original monazite, such that newly precipitated monazite may copy or partly inherit the age of a precursor grain. This implies that monazite grown via coupled dissolution-precipitation may not faithfully record the age or duration of metamorphism in melt-bearing rocks typical of a variety of geodynamic settings.
dc.description.statementofresponsibilityJan Varga, Tom Raimondo, Nathan R.Daczko, John Adam
dc.identifier.citationChemical Geology, 2020; 544:1-16
dc.identifier.doi10.1016/j.chemgeo.2020.119602
dc.identifier.issn0009-2541
dc.identifier.issn1872-6836
dc.identifier.orcidRaimondo, T. [0000-0001-9115-9196]
dc.identifier.urihttp://hdl.handle.net/2440/126941
dc.language.isoen
dc.publisherElsevier
dc.relation.granthttp://purl.org/au-research/grants/arc/DP160103449
dc.rights© 2020 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.chemgeo.2020.119602
dc.subjectMonazite; experimental petrology; U–Th–Pb; coupled dissolution-precipitation; metamorphism
dc.titleExperimental alteration of monazite in granitic melt: Variable U–Th–Pb and REE mobility during melt-mediated coupled dissolution-precipitation
dc.typeJournal article
pubs.publication-statusPublished

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