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Monazite and xenotime petrogenesis in the contact aureole of the Makhavinekh Lake Pluton, northern Labrador

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dc.contributor.authorMcFarlane, Christopher
dc.contributor.authorConnelly, J-P
dc.contributor.authorCarlson, W
dc.date.accessioned2015-12-13T23:08:59Z
dc.date.issued2005
dc.date.updated2015-12-12T08:16:59Z
dc.description.abstractHigh-temperature (700-900°C) metamorphism in the contact aureole of the Makhavinekh Lake Pluton (MLP), northern Labrador, led to the growth of monazite and xenotime during progressive replacement of regional garnet-bearing assemblages (M1) by lower-press
dc.identifier.issn0010-7999
dc.identifier.urihttp://hdl.handle.net/1885/86809
dc.publisherSpringer
dc.sourceContributions to Mineralogy and Petrology
dc.subjectKeywords: aureole; metamorphism; monazite; petrogenesis; xenotime; Canada; Labrador; Makhavinekh Lake; Newfoundland and Labrador; North America; Western Hemisphere; World
dc.titleMonazite and xenotime petrogenesis in the contact aureole of the Makhavinekh Lake Pluton, northern Labrador
dc.typeJournal article
local.bibliographicCitation.lastpage541
local.bibliographicCitation.startpage524
local.contributor.affiliationMcFarlane, Christopher, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationConnelly, J-P, University of Texas
local.contributor.affiliationCarlson, W, University of Texas
local.contributor.authoruidMcFarlane, Christopher, u4071989
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040203 - Isotope Geochemistry
local.identifier.absfor040304 - Igneous and Metamorphic Petrology
local.identifier.ariespublicationMigratedxPub15822
local.identifier.citationvolume148
local.identifier.doi10.1007/s00410-004-0618-7
local.identifier.scopusID2-s2.0-11444255051
local.type.statusPublished Version

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