2015
DOI: 10.1016/j.oregeorev.2014.06.001
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Corrigendum to “Evolution of rare-earth mineralization in the Bear Lodge carbonatite, Wyoming: Mineralogical and isotopic evidence” [Ore Geol. Rev. 64 (2015) 499–521]

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Cited by 2 publications
(3 citation statements)
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“…Field IV: calcite-ankerite-dolomite and dolomite carbonatites and siderite (spherolite and oolite) rocks. The trends III and IV correlate well with the hydrothermal trend and with the trend that represents interaction of alkaline rocks and carbonatite with meteoric water [14]. Field V: Proterozoic and Cambrian sedimentary carbonates, including marbled carbonates of the Ulakhan-Kurung Fm.…”
Section: Discussionsupporting
confidence: 63%
“…Field IV: calcite-ankerite-dolomite and dolomite carbonatites and siderite (spherolite and oolite) rocks. The trends III and IV correlate well with the hydrothermal trend and with the trend that represents interaction of alkaline rocks and carbonatite with meteoric water [14]. Field V: Proterozoic and Cambrian sedimentary carbonates, including marbled carbonates of the Ulakhan-Kurung Fm.…”
Section: Discussionsupporting
confidence: 63%
“…Naturally formed cerianite has been found: (1) in association with bastnasite/monazite; 31–36 (2) as a secondary mineral, as a result of hydrothermally-altered carbonate/apatite weathering; 2,31,37,38 (3) replacing early crystallised ancylite and fluorocarbonates; 40 (4) as an overgrowth on Ce-depleted monazite. 40 Our experiments explain these findings in natural deposits and are consistent with the decarbonation processes of rare earth carbonates due to the crystallisation of Ce-carbonates under low-hydrothermal conditions (35–205 °C). Consequently, Ce-rich carbonates will tend to be unstable in carbonate deposits with large concentrations of Ce under hydrothermal conditions.…”
Section: Implications For Natural Systems and Industrymentioning
confidence: 99%
“…Similarly, Zaitsev et al 39 found that cerianite formed during the alteration of apatite as a result of carbonate weathering precipitated from groundwater. Moore et al 40 reported cerianite in Bear Lodge carbonatite, Wyoming, USA, that partially replaced early-crystallised ancylite and fluorocarbonates; they also observed Ce-depleted monazite in association with cerianite at certain localities. Van Rythoven et al , 38 studied the same carbonatite and found that hydrothermally-altered carbonatite with unoxidized REEs occurs primarily as ancylite and parisite-synchysite, while monazite, bastnasite, and cerianite were labeled as subordinate minerals, broken down by supergene oxidation.…”
Section: Introductionmentioning
confidence: 99%