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• W2285407029 abstract "The Lala Fe-Cu-(Mo, REE) deposit in the northern Kangdian IOCG metallogenic province, SW China, has a paragenetic sequence that includes pre-ore Na-alteration (Stage I), Fe-(P) mineralization (Stage II), and sulfide mineralization (Stage III). Rare earth element (REE) minerals, which are chiefly monazite, parasite, and bastnäsite with minor xenotime, are associated with sulfide mineralization. These REE minerals, together with biotite, muscovite, and calcite, are accompanied with K-Ca-carbonate alteration of Stage III. Where magnetite and apatite of Stage II are overprinted by minerals of Stage III, the apatite grains are commonly embayed or eroded and contain abundant rounded to subrounded and needle-like inclusions of monazite and minor bastnäsite, calcite, and sulfide minerals. These monazite-bearing apatite grains are texturally similar to metasomatized apatite in the laboratory, and can be attributed to the formation from Stage II apatite via a dissolution-precipitation process during fluid infiltration. The monazite-bearing apatite has REE contents and La/Sm ratios much lower than the original Stage II apatite, suggesting that REEs were leached and mobilized from this Stage II apatite, and that these processes were responsible for the formation of monazite inclusions within the apatite hosts. The monazite inclusions have compositions similar to those of Stage III monazite, suggesting that REEs in Stage II apatite were mobilized by Stage III fluids, consistent with occurrences of sulfide and calcite inclusions within the apatite. Mass balance analysis using bulk compositional data for host rocks that underwent K-Ca-carbonate alteration indicates that REEs of the hosting rocks were also mobilized, and that up to 70 percent of the light REEs were leached out during alteration. Therefore, REE mobilization recorded in apatite grains and country rocks support a model in which the country rocks were important sources for REEs in the Lala deposit. Compositions of amphibole and biotite, together with previously acquired fluid inclusion data, demonstrate that Stage III fluids are dominated by Na^+^ and Cl^−^ but had higher K, CO~2~ (or HCO~3~^−^ and CO~3~^2−^), and HF/HCl fugacity and lower salinity (NaCl) than Stage II fluids. Elevated K and CO~2~ in Stage III fluids, or associated K-carbonate alteration, is proposed to be important for extensive REE mobilization on country rocks. The REEs leached from country rocks are inferred to have been transported as chloride complexes prior to being deposited as REE minerals. Deposition of REE minerals from Stage III fluids was likely triggered by mixing with external, relatively low temperature, F-rich, and high-pH fluids and/or by local interaction with carbonate host rocks. We suggest that the common association of REEs with Cu ores in many IOCG deposits is related to the unique nature of the Cu mineralizing fluids." @default.
• W2285407029 created "2016-06-24" @default.
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• W2285407029 creator A5082651070 @default.
• W2285407029 date "2015-08-05" @default.
• W2285407029 modified "2023-09-30" @default.
• W2285407029 title "Mineralogical and geochemical constraints on mobilization and mineralization of rare Earth elements in the Lala Fe-Cu-(Mo, Ree) deposit, SW China" @default.
• W2285407029 cites W135524032 @default.
• W2285407029 cites W1976594053 @default.
• W2285407029 cites W1977323507 @default.
• W2285407029 cites W1978466946 @default.
• W2285407029 cites W1978484550 @default.
• W2285407029 cites W1982272146 @default.
• W2285407029 cites W1982824385 @default.
• W2285407029 cites W1986876280 @default.
• W2285407029 cites W1988702169 @default.
• W2285407029 cites W1995585326 @default.
• W2285407029 cites W1998026152 @default.
• W2285407029 cites W1999369100 @default.
• W2285407029 cites W1999726370 @default.
• W2285407029 cites W2003817890 @default.
• W2285407029 cites W2004935853 @default.
• W2285407029 cites W2006593586 @default.
• W2285407029 cites W2008632542 @default.
• W2285407029 cites W2011270892 @default.
• W2285407029 cites W2014200433 @default.
• W2285407029 cites W2018418225 @default.
• W2285407029 cites W2024236183 @default.
• W2285407029 cites W2024436619 @default.
• W2285407029 cites W2027731616 @default.
• W2285407029 cites W2031057485 @default.
• W2285407029 cites W2033352261 @default.
• W2285407029 cites W2038019149 @default.
• W2285407029 cites W2040688553 @default.
• W2285407029 cites W2041219564 @default.
• W2285407029 cites W2055027691 @default.
• W2285407029 cites W2055264330 @default.
• W2285407029 cites W2060333503 @default.
• W2285407029 cites W2061178090 @default.
• W2285407029 cites W2065928479 @default.
• W2285407029 cites W2070466214 @default.
• W2285407029 cites W2073134412 @default.
• W2285407029 cites W2076179867 @default.
• W2285407029 cites W2077835903 @default.
• W2285407029 cites W2083808432 @default.
• W2285407029 cites W2084165122 @default.
• W2285407029 cites W2087335223 @default.
• W2285407029 cites W2087494921 @default.
• W2285407029 cites W2092241581 @default.
• W2285407029 cites W2096775033 @default.
• W2285407029 cites W2104287039 @default.
• W2285407029 cites W2108538927 @default.
• W2285407029 cites W2112052324 @default.
• W2285407029 cites W2127236625 @default.
• W2285407029 cites W2127641354 @default.
• W2285407029 cites W2127650401 @default.
• W2285407029 cites W2133678589 @default.
• W2285407029 cites W2138522501 @default.
• W2285407029 cites W2152195282 @default.
• W2285407029 cites W2167450488 @default.
• W2285407029 cites W2168661179 @default.
• W2285407029 cites W2168779027 @default.
• W2285407029 cites W2170646720 @default.
• W2285407029 cites W2199969768 @default.
• W2285407029 cites W2303568235 @default.
• W2285407029 cites W2315476094 @default.
• W2285407029 cites W2326411402 @default.
• W2285407029 cites W2327214248 @default.
• W2285407029 cites W2330293686 @default.
• W2285407029 cites W2341661556 @default.
• W2285407029 cites W2351956331 @default.
• W2285407029 cites W2353870592 @default.
• W2285407029 cites W2356798643 @default.
• W2285407029 cites W2358216271 @default.
• W2285407029 cites W2365053346 @default.
• W2285407029 cites W2373371179 @default.
• W2285407029 cites W2473805362 @default.
• W2285407029 cites W2484344076 @default.
• W2285407029 cites W2947596473 @default.
• W2285407029 cites W3203664529 @default.
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• W2285407029 doi "https://doi.org/10.2475/07.2015.03" @default.
• W2285407029 hasPublicationYear "2015" @default.
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