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Melluso, Leone, Guarino, Vincenza, Lustrino, Michele, Morra, Vincenzo, de' Gennaro, Roberto (2017) TheREE-and HFSE-bearing phases in the Itatiaia alkaline complex (Brazil) and geochemical evolution of feldspar-rich felsic melts. Mineralogical Magazine, 81 (2) 217-250 doi:10.1180/minmag.2016.080.122

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Reference TypeJournal (article/letter/editorial)
TitleTheREE-and HFSE-bearing phases in the Itatiaia alkaline complex (Brazil) and geochemical evolution of feldspar-rich felsic melts
JournalMineralogical Magazine
AuthorsMelluso, LeoneAuthor
Guarino, VincenzaAuthor
Lustrino, MicheleAuthor
Morra, VincenzoAuthor
de' Gennaro, RobertoAuthor
Year2017 (April)Volume81
Issue2
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2016.080.122Search in ResearchGate
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Mindat Ref. ID244883Long-form Identifiermindat:1:5:244883:5
GUID0
Full ReferenceMelluso, Leone, Guarino, Vincenza, Lustrino, Michele, Morra, Vincenzo, de' Gennaro, Roberto (2017) TheREE-and HFSE-bearing phases in the Itatiaia alkaline complex (Brazil) and geochemical evolution of feldspar-rich felsic melts. Mineralogical Magazine, 81 (2) 217-250 doi:10.1180/minmag.2016.080.122
Plain TextMelluso, Leone, Guarino, Vincenza, Lustrino, Michele, Morra, Vincenzo, de' Gennaro, Roberto (2017) TheREE-and HFSE-bearing phases in the Itatiaia alkaline complex (Brazil) and geochemical evolution of feldspar-rich felsic melts. Mineralogical Magazine, 81 (2) 217-250 doi:10.1180/minmag.2016.080.122
Abstract/NotesAbstractThe Late Cretaceous Itatiaia complex is made up of nepheline syenite grading to peralkaline varieties, quartz syenite and granite, emplaced in the metamorphic rocks of the Serra do Mar, SE Brazil. The nepheline syenites are characterized by assemblages with alkali feldspar, nepheline, Fe-Ti oxides, clinopyroxene, amphibole, apatite and titanite, while the peralkaline nepheline syenites have F-disilicates (rinkite, wöhlerite, hiortdahlite, lÄvenite), britholite and pyrophanite as the accessory phases. The silica-oversaturated rocks have alkali feldspar, plagioclase, quartz, amphibole, clinopyroxene and Fe-Ti oxides; the chevkinite-group minerals are the featured accessory phases and are found with allanite, fluorapatite, fluorite, zircon, thorite, yttrialite, zirconolite, pyrochlore and yttrocolumbite. The major- and trace-element composition of the Itatiaia rocks have variations linked to the amount of accessory phases, have smooth, enriched chondritenormalized rare-earth element (REE) distribution patterns in the least-evolved nepheline syenites and convex patterns in the most-evolved nepheline syenites. The REE distribution patterns of the quartz syenites and granites show a typical pattern caused by fractional crystallization of feldspar and amphibole, in an environment characterized by relatively high oxygen fugacity (>NiNiO buffer) and high concentrations of H2O and F, supporting the crystallization of hydrous phases, fluorite and F-disilicates. The removal of small amounts of titanite in the transition from the least-evolved to the most-evolved nepheline syenites stems from petrogenetic models involving REE, and is shown to be a common feature of the magmatic evolution of many other syenitic/ trachytic/ phonolitic complexes of the Serra do Mar and elsewhere.

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LocalityCitation Details
Itatiaia alkaline complex, Itatiaia, Rio de Janeiro, Brazil

Mineral Occurrences

LocalityMineral(s)
Itatiaia alkaline complex, Itatiaia, Rio de Janeiro, Brazilⓘ Allanite Group, ⓘ Amphibole Supergroup, ⓘ Apatite, ⓘ Chevkinite Group, ⓘ Clinopyroxene Subgroup, ⓘ Fluorapatite, ⓘ Fluorite, ⓘ Hiortdahlite, ⓘ K Feldspar, ⓘ LĂ„venite, ⓘ Nepheline, ⓘ Plagioclase, ⓘ Pyrochlore Group, ⓘ Pyrophanite, ⓘ Quartz, ⓘ Rinkite-(Ce), ⓘ Thorite, ⓘ Titanite, ⓘ Wöhlerite, ⓘ Yttrialite-(Y), ⓘ Yttrocolumbite-(Y), ⓘ Zircon, ⓘ Zirconolite


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