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Significance of apatite REE depletion and monazite inclusions in the brecciated Se-Chahun iron oxide-apatite deposit, Bafq district, Iran: Insights from paragenesis and geochemistry

Citation

Bonyadi, Z and Davidson, GJ and Mehrabi, B and Meffre, S and Ghazban, F, Significance of apatite REE depletion and monazite inclusions in the brecciated Se-Chahun iron oxide-apatite deposit, Bafq district, Iran: Insights from paragenesis and geochemistry, Chemical Geology: An International Journal, 281, (3-4) pp. 253-269. ISSN 0009-2541 (2011) [Refereed Article]


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DOI: doi:10.1016/j.chemgeo.2010.12.013

Abstract

The Se–Chahun magnetite–apatite deposit (Bafq district, central Iran) comprises several orebodies with largescale replacement and brecciation textures, and a sodic–calcic alteration envelope. Such members of the ironoxide copper–gold (IOCG) deposit family commonly exhibit REE enrichment, but the source and evolution of the REE component is arguable. In the Anomaly X orebody, semi-massive ilmenite-rich magnetite and coarse REE-rich fluorapatite formed at 510±8 Ma (U–Pb LA-ICPMS age), at the end of the main regional sodic magmatic event (525±7 Ma). Prior to a major brecciation, a metasomatic event removed Ti and Al from magnetite grain boundaries, and leached primary fluorapatite (BSE-bright) of LREE, Y, Na, Cl, Mg, Mn and Fe, leaving BSE-dark apatite that contained LREE-rich monazite and co-existing vapor- and liquid-dominated fluid inclusions. Subsequent brecciation and hydrothermal infill produced a matrix dominated by actinolite, K-feldspar, biotite, chlorite, calcite, hematite, rutile, and titanite, but apatite was not further metasomatized. It is concluded that P, REE, Ti, Al and Fe were readily transported in the early sodic–calcic fluids, but P and the REE had very restricted mobility (mm's to cm's) in the CO2–K–Cl-rich fluids responsible for apatite metasomatism. A role for fluid over-pressuring as a means of increasing the efficacy of apatite REE leaching is circumstantially suggested by the observation that the metasomatic event was terminated by tensile failure. Overall, a case is emerging for fluid-induced nucleation of monazite, and accompanying apatite REE depletion, to be included as a typical but subtle paragenetic feature within the iron oxide–apatite deposit model.

Item Details

Item Type:Refereed Article
Keywords:iron oxide–apatite deposit, Iran, monazite, rare earth elements, Bafq Mineral Province, Pb-isotopes
Research Division:Earth Sciences
Research Group:Geochemistry
Research Field:Geochemistry not elsewhere classified
Objective Division:Mineral Resources (excl. Energy Resources)
Objective Group:Mineral Exploration
Objective Field:Copper Ore Exploration
Author:Davidson, GJ (Dr Garry Davidson)
Author:Meffre, S (Dr Sebastien Meffre)
ID Code:74771
Year Published:2011
Web of Science® Times Cited:60
Deposited By:Centre for Ore Deposit Research - CODES CoE
Deposited On:2011-12-13
Last Modified:2012-12-13
Downloads:7 View Download Statistics

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