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fluorocarbonates

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Journal Article
Published: 01 July 2014
American Mineralogist (2014) 99 (7): 1335–1346.
... into the short-wave infrared. These REE fluorocarbonate mineral samples were characterized via scanning electron microscopy and electron probe microanalysis. Sharp absorptions of REE-bearing minerals are mostly the result of 4 f -4 f intraconfigurational electron transitions and for the light REE-enriched...
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Series: GSA Engineering Geology Case Histories
Published: 01 January 1978
DOI: 10.1130/Eng-Case-11.73
EISBN: 9780813759364
... not proportionally increase the soundness. The soundness was improved in fluorocarbon-acrylic copolymers, but here the chemical improvement was at its best. The maximum improvement of soundness was experienced by epoxy-treated specimens. An absolute prediction of the long-range behavior of preservative treatments...
Journal Article
Published: 01 March 1991
The Canadian Mineralogist (1991) 29 (1): 107–111.
Image
Back-scattered electron images: REE fluorocarbonates from hydrothermal veins in BIT carbonatite stockwork. The small bright spots within the fluorocarbonates are the target microprobe beam. Brighter areas (higher-Z areas) are barite, and darker areas (lower-Z areas) are quartz, carbonates and fluorite, except for the image A, which is made with reverse contrast. A (BIT5/61.20). Overview of fibroradial aggregates of synchysite, parisite and bastnäsite in vein mainly consisting of quartz, barite and fluorite (reverse contrast). B (BIT2/75.65; anal. 15 to 18). Fibroradial aggregates of synchysite (gray). Large crystals of barite (bright) are in the upper part of the image. C (BIT5/40.00; anal. 10 to 12). Large laths of synchysite (gray) with thin parisite layers (light gray). Toward the NW corner of the image, one can see the parisite layer along the fracture in the synchysite. D (BIT5/40.00; anal. 13). Laths of synchysite (gray) associated with layers of parisite (light gray). E (BIT5/40.00; anal. 14). Laths of synchysite (gray) with very fine layers of parisite (light gray), between barite (bright) and fluorite (dark). F (BIT5/61.20; anal. 21 to 26). Synchysite–parisite syntactic intergrowths (gray) in aggregates of fibers radiating from a common nucleus of bastnäsite (bright). Also to be observed is a texture very similar to that shown in image B. G (BIT5/61.20; anal. 4 to 5). Radial laths of synchysite with very fine layers of parisite. H (BIT5/61.20; anal. 7 to 9). Prismatic crystals of synchysite with thin layers of parisite.
Published: 01 August 2008
F ig . 5. Back-scattered electron images: REE fluorocarbonates from hydrothermal veins in BIT carbonatite stockwork. The small bright spots within the fluorocarbonates are the target microprobe beam. Brighter areas (higher-Z areas) are barite, and darker areas (lower-Z areas) are quartz
Image
Published: 01 October 2007
TABLE 1. CHEMICAL COMPOSITION OF FLUOROCARBONATES
Journal Article
Published: 01 August 2008
The Canadian Mineralogist (2008) 46 (4): 901–914.
...F ig . 5. Back-scattered electron images: REE fluorocarbonates from hydrothermal veins in BIT carbonatite stockwork. The small bright spots within the fluorocarbonates are the target microprobe beam. Brighter areas (higher-Z areas) are barite, and darker areas (lower-Z areas) are quartz...
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Journal Article
Published: 01 December 1997
American Mineralogist (1997) 82 (11-12): 1255–1260.
Journal Article
Published: 01 February 1997
The Canadian Mineralogist (1997) 35 (1): 181–187.
Journal Article
Published: 01 June 1997
The Canadian Mineralogist (1997) 35 (3): 743–749.
Image
Rare earth fluorocarbonate textural relationships. A) Backscattered electron (BSE) image of synchysite/parisite (gray) with bastnäsite cores (white). B) BSE image of rare earth element (REE)-fluorocarbonates (mainly synchysite/parisite) intergrown with barite. C) BSE image of REE-fluorocarbonates intergrown with pyrite and partially intergrown with Nb-bearing TiO2 polymorphs and calcite. D) REE-fluorocarbonates intergrown with pyrite in association with strontianite and ancylite (reflected and transmitted light in plane-polarized light). Abbreviations: anc = ancylite, bast = bastnäsite, brt = barite, cal = calcite, Rfc = REE-fluorocarbonate, py = pyrite, str = strontianite, syn = synchysite/parasite, Ti-ox = TiO2 polymorph.
Published: 01 June 2022
Fig. 6. Rare earth fluorocarbonate textural relationships. A) Backscattered electron (BSE) image of synchysite/parisite (gray) with bastnäsite cores (white). B) BSE image of rare earth element (REE)-fluorocarbonates (mainly synchysite/parisite) intergrown with barite. C) BSE image of REE
Journal Article
Published: 01 February 1998
Mineralogical Magazine (1998) 62 (1): 55–64.
...Xiuling Wu; Dawei Meng; Zhaolu Pan; Guangming Yang; Douxing Li Structures of calcium-rare-earth (Ca-RE) fluorocarbonate minerals from southwest China have been investigated using selected area electron diffraction (SAED) and high-resolution transmission electron microscopy (HRTEM...
Journal Article
Published: 01 January 2025
Jour. Geol. Soc. India (2025) 101 (1): 87–96.
... and chevkinite is responsible for the enrichment of ΣLREE (Max.1645ppm) over ΣHREE (Max.129ppm) in Podili syenite evolved through volatile enriched Podili alkali granite. Enrichment of fluorocarbonate bastnaesite indicates the presence of halogen F- in the melt, which substitutes hydroxyl ion (OH...
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Journal Article
Published: 03 July 2023
American Mineralogist (2023) 108 (7): 1298–1314.
... Jiufeng granite in the Zhuguangshan batholith, South China. Alteration of allanite in the Changjiang granite is characterized by the altered domains with lower backscattered electron (BSE) intensities than the unaltered domains and replacement by other secondary minerals such as REE fluorocarbonates...
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Journal Article
Published: 01 January 2019
The Canadian Mineralogist (2019) 57 (1): 3–24.
... are steeply downwards-sloping with a relatively low and flat HREE segment. Such a fractionation trend is markedly different from that seen for REE-fluorocarbonates, the dominant REE host at Olympic Dam, which contain relatively higher MREE and HREE components. Xenotime is relatively rare at Olympic Dam...
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Image
Backscattered electron (BSE) images of rare earth minerals. A) Strontianite replacement of rare earth element (REE)-fluorocarbonates and ancylite. B) Replacement of daqingshanite by SCRp in association with ancylite and strontianite within a rare earth pseudomorph. C) Evidence of SCRp replacement of ancylite. D) Subhedral, wedge-shaped, and compositionally zoned SCRp. Abbreviations: anc = ancylite, cal = calcite, dq = daqingshanite, Rfc = REE-fluorocarbonate, SCRp = Sr-Ca-REE-phosphate, str = strontianite.
Published: 01 June 2022
Fig. 7. Backscattered electron (BSE) images of rare earth minerals. A) Strontianite replacement of rare earth element (REE)-fluorocarbonates and ancylite. B) Replacement of daqingshanite by SCRp in association with ancylite and strontianite within a rare earth pseudomorph. C) Evidence of SCRp
Image
Micron- to submicron-sized rare earth element (REE) fluorocarbonate inclusions in dolomite (Dol) (A-C) and calcite (Cal) (D-F). (A) Submicron-sized REE fluorocarbonate grains (tiny bright spots) occurring within a thin veinlet of dolomite. (B) Comparatively larger synchysite-(Ce) (Syn) grains within dolomite. (C) Synchysite-(Ce) inclusions in larger patches of dolomite that replaced primary ankerite (Ank). (D) Synchysite-(Ce) inclusions in a large calcite (Cal1) that has been replaced by Fe (hydr)oxides and fluorite (Fl) along grain boundaries. (E) Intergrowth of parisite-(Ce), synchysite-(Ce), florencite-(Ce) (Fln), and barite (Brt) in a calcite-dominated matrix. (F) Intergrowth of synchysite and barite, surrounded by altered calcite (Cal2) containing small inclusions of Fe (hydr)oxide and REE fluorocarbonates in a fluorite- and quartz-dominated matrix. Note the syntactic intergrowth between parisite-(Ce) and synchysite-(Ce) in (E), wherein the former occurs as thin needles in the latter. The scale bars in (A) through (F) are 50 μm.
Published: 01 May 2022
Fig. 9. Micron- to submicron-sized rare earth element (REE) fluorocarbonate inclusions in dolomite (Dol) (A-C) and calcite (Cal) (D-F). (A) Submicron-sized REE fluorocarbonate grains (tiny bright spots) occurring within a thin veinlet of dolomite. (B) Comparatively larger synchysite-(Ce) (Syn
Image
Backscattered electron and X-ray WDS element maps of eudialyte pseudomorphs. (A) Sample L10-269-254.96 (uncalibrated, brighter colors correspond to higher concentrations). Yttrium indicates the distribution of fergusonite-(Y) and samarskite-(Y); Nd that of LREE minerals, mainly REE-fluorocarbonates. (B) Sample L10-267-253.54. Zircon, fergusonite-(Y), and samarskite-(Y) are restricted to the interior of the pseudomorphs, whereas REE-fluorocarbonates, such as bastnäsite-(Ce), occur throughout the sample.
Published: 01 December 2017
-fluorocarbonates. (B) Sample L10-267-253.54. Zircon, fergusonite-(Y), and samarskite-(Y) are restricted to the interior of the pseudomorphs, whereas REE-fluorocarbonates, such as bastnäsite-(Ce), occur throughout the sample.
Image
SEM images of significant mineral phases in studied slates. (a–c) Luarca slate ((a) pyrrhotite; (b) REE-rich fluorocarbonate (white); (c) titanium dioxide mineral, probably anatase); (d–f) Culm slate ((d) well-formed pyrite framboid; (e) REE-rich fluorocarbonate (light grey) and REE phosphate (white); (f) zircon). Images (a)–(c), (e) and (f) were taken in BSE mode; (d) is a secondary electron image.
Published: 19 February 2018
Fig. 7. SEM images of significant mineral phases in studied slates. ( a – c ) Luarca slate (( a ) pyrrhotite; ( b ) REE-rich fluorocarbonate (white); ( c ) titanium dioxide mineral, probably anatase); ( d – f ) Culm slate (( d ) well-formed pyrite framboid; ( e ) REE-rich fluorocarbonate (light
Image
Chondrite-normalized rare-earth element profiles of fluoride melt inclusions (FMs). The chondrite-normalization values are from Sun and McDonough (1989). The abbreviations are as follows: FM cont. Flc = fluoride melt inclusion containing fluorocarbonate mineral.
Published: 01 March 2025
Fig. 16. Chondrite-normalized rare-earth element profiles of fluoride melt inclusions (FMs). The chondrite-normalization values are from Sun and McDonough ( 1989 ). The abbreviations are as follows: FM cont. Flc = fluoride melt inclusion containing fluorocarbonate mineral.
Journal Article
Journal: Economic Geology
Published: 01 May 2022
Economic Geology (2022) 117 (3): 683–702.
...Fig. 9. Micron- to submicron-sized rare earth element (REE) fluorocarbonate inclusions in dolomite (Dol) (A-C) and calcite (Cal) (D-F). (A) Submicron-sized REE fluorocarbonate grains (tiny bright spots) occurring within a thin veinlet of dolomite. (B) Comparatively larger synchysite-(Ce) (Syn...
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