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

• Published in: Chemical geology Vol. 281; no. 3; pp. 253 - 269
• Main Authors: Bonyadi, Zahra, Davidson, Garry J., Mehrabi, Behzad, Meffre, Sebastien, Ghazban, Fereydoun
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 24.02.2011
• Subjects: aluminum; Apatite; Bafq Mineral Province; biotite; calcite; Computational fluid dynamics; Deposits; Fluid flow; Fluids; geochemistry; hematite; Iran; iron; Iron oxides; Iron oxide–apatite deposit; leaching; magnesium; Magnetite; manganese; Monazite; Pb-isotopes; Rare earth elements; sodium; Texture; Iran; ISW, Iran; Bafq Mineral Province; Iran; Rare earth elements; Pb-isotopes; Iron oxide–apatite deposit; Monazite
• ISSN: 0009-2541; 1872-6836
• DOI: 10.1016/j.chemgeo.2010.12.013

The Se–Chahun magnetite–apatite deposit (Bafq district, central Iran) comprises several orebodies with large-scale replacement and brecciation textures, and a sodic–calcic alteration envelope. Such members of the iron-oxide 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 CO 2–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. ► Apatite metasomatism occurs due to fluid over-pressuring immediately prior to brecciation. ► Apatite metasomatism is the first consequence of a shift to K-rich fluids in the system. ► The genetic affinity of the apatites is still recognisable on a Y–Sr classification diagram despite significant removal of LREE. ► Apatite first formed at 510 ± 8 Ma, at the end of or after regional sodic granite intrusion in the BMP. ► Pre-brecciation metasomatism leached the margins of magnetite crystals of Ti and Al.