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cheralite

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Journal Article
Published: 01 August 2008
American Mineralogist (2008) 93 (8-9): 1356–1362.
...Karin Popa; Tatiana Shvareva; Lena Mazeina; Eric Colineau; Franck Wastin; Rudy J.M. Konings; Alexandra Navrotsky Abstract The mineral cheralite [CaTh(PO 4 ) 2 ] allows for the incorporation of tetravalent actinides in monazite-based crystalline phases. Experimental determination of its...
FIGURES
Journal Article
Published: 01 June 2007
The Canadian Mineralogist (2007) 45 (3): 503–508.
...Kees Linthout Abstract The nomenclature for the system 2REEPO 4 – CaTh(PO 4 ) 2 – 2ThSiO 4 has been revised, to be consistent with CNMMN principles. Henceforth, only three names will be applied to members dominated by the respective end-member compositions monazite, cheralite, and huttonite...
FIGURES
Journal Article
Published: 01 February 1967
American Mineralogist (1967) 52 (1-2): 13–19.
...J. J. Finney; N. Nagaraja Rao Abstract The structure of cheralite, a thorium, calcium, rare earth monazite, has been completely redetermined. Patterson sections and three-dimensional difference maps were used to determine the atomic positions, and least squares refinement of the data reduced the R...
Journal Article
Published: 01 April 1965
American Mineralogist (1965) 50 (3-4): 507–508.
...N. Nagaraja Rao; J. J. Finney Abstract Bowie and Horne (1953) described cheralite as a green mineral belonging to the monazite group intermediate in composition between monazite and the compound CaTh(PO 4 ) 2 . They presented chemical analyses from two supposedly different localities: Kuttakuzhi...
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Ternary diagrams (LREE) – (HREE+Y) – (thorite&#x2F;huttonite+<span class="search-highlight">cheralite</span>) for ( a ...
Published: 01 July 2013
Figure 4 Ternary diagrams (LREE) – (HREE+Y) – (thorite/huttonite+cheralite) for ( a ) monazite detrital core, ( b ) rim, and ( c ) xenotime.
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Nomenclature diagram for the system monazite (2 REE PO 4 )-<span class="search-highlight">cheralite</span> (CaTh(...
Published: 01 August 2007
F ig . 6. Nomenclature diagram for the system monazite (2 REE PO 4 )-cheralite (CaTh(PO 4 ) 2 )-huttonite (2ThSiO 4 ) (after Linthout, 2007 ). When calculating the end-member proportions, U and Fe are combined with CaTh(PO 4 ) 2 ; any remaining Th is combined with Si in ThSiO 4 ; Y is included
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COMPOSITIONS OF TYPE <span class="search-highlight">CHERALITE</span> AND OF DISCREDITED TYPE BRABANTITE
Published: 01 June 2007
TABLE 2. COMPOSITIONS OF TYPE CHERALITE AND OF DISCREDITED TYPE BRABANTITE
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SEM-BSE image of the studied crystal. ( a ) general view; ( b ) enlargement...
Published: 01 December 2004
F ig . 2. SEM-BSE image of the studied crystal. ( a ) general view; ( b ) enlargement showing the cheralite crystals; ( c ) further enlargement showing the baddeleyite skeleton (bd) covered with cheralite (ch) and uraninite (u); ( d ) detail of the betafite crystal covered with cheralite.
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Dominant element substitutions in monazite from the study area. ( a ) Plot ...
Published: 01 August 2007
F ig . 8. Dominant element substitutions in monazite from the study area. ( a ) Plot of Si+Ca vs . Th+U shows obvious linear correlation indicating that both cheralite ((Th,U)Ca(PO 4 ) 2 ) and huttonite ((Th,U)SiO 4 ) contribute to the element substitutions. ( b ) and ( c ) show that cheralite
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Variation in monazite composition. (A) Ternary diagram highlighting differe...
Published: 13 April 2017
Figure 8. Variation in monazite composition. (A) Ternary diagram highlighting differences in monazite-xenotime (REEPO 4 ), cheralite-huttonite (Ca,Th)(P,Si)O 4 , and anhydrite-celestine (Ca,Sr)SO 4 components. This latter was calculated based solely on the measured S content in order
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Binary exchange vector diagram with the composition of the analysed monazit...
Published: 01 October 2009
Fig. 3. Binary exchange vector diagram with the composition of the analysed monazites, based on calculation of 16 oxygen per formula unit, with exchange vectors from pure monazite towards the cheralite and huttonite end-members indicated by arrows. All data lie between these two substitution
Journal Article
Published: 01 October 2012
The Canadian Mineralogist (2012) 50 (5): 1331–1346.
... ilmenite-series granitic pegmatite. The observed variations in their chemical composition are largely explained by the huttonite exchange [(Th + U) 4+ ↔Si 4+ ], and subordinately by the cheralite exchange [(Th + U) 4+ ↔2Ca 2+ ]. However, there are differences in the degree of contribution of the two...
FIGURES | View All (8)
Journal Article
Published: 01 April 1998
American Mineralogist (1998) 83 (3-4): 259–272.
... of brabantite and the first occurrence of this mineral in a granite. Many new occurrences of cheralite-(Ce), as well as a monazite-group mineral intermediate between monazite-(Ce) and huttonite for which the term huttonitic monazite is proposed, were discovered. Even "common" monazite-(Ce) may show extreme...
Journal Article
Published: 01 August 1978
American Mineralogist (1978) 63 (7-8): 757–761.
... percent) is also present; silica is nearly absent (0.16 percent). From these data, relationships to cheralite are evident, and the mineral might be considered as a uranium-rich cheralite, or as its uranium-bearing equivalent; the name monazite is used on account of the ratio (Ca + U + Th)/(Ce + La + Pr...
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SEM-BSE images showing ( a ) altered sodalite, with small pyrite crystals a...
Published: 01 December 2004
F ig . 1. SEM-BSE images showing ( a ) altered sodalite, with small pyrite crystals aligned along crystallographic planes; ( b ) association of apatite (dark grey) , britholite (light grey) and cheralite (acicular, light-grey crystals); ( c ) very small acicular zirconolite within K-feldpar; ( d
Journal Article
Published: 01 July 2016
American Mineralogist (2016) 101 (7): 1604–1623.
..., and contains up to 44.88% TiO 2 , 3.12% Nb 2 O 5 , 6.52% Y 2 O 3 , 0.80% Dy 2 O 3 , 2.63% ThO 2 , 6.0% P 2 O 5 , and 3.73% F. Electron microprobe analyses of xenotime-(Y) overgrowths on zircon show that oscillatory zoning is a result of variable Th and Ca content. Cheralite-type substitution, whereby Th and Ca...
FIGURES | View All (10)
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Monazite composition in samples from the Shimokuhara (SHK, SHK2) and Namera...
Published: 01 April 2020
samples, and the dominant cheralitic substitution for secondary domain analyses in NAM. ( b ) Y vs. U diagram (cation fraction on A site) showing Y-U depletion for some secondary domain analyses in SHK, and Y-U enrichment for secondary domain analyses in NAM. ( c ) Ternary diagram showing proportions
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(a) Graph of 4*(P + Y + ΣREE)  versus  4*(Si + Th + U)  apfu  for monazite–...
Published: 01 July 2016
Fig. 4. (a) Graph of 4*(P + Y + ΣREE) versus 4*(Si + Th + U) apfu for monazite–cheralite–huttonite (after Harlov et al . 2008 ); note that all the studied monazite-(Ce) falls within the monazite field, variably enriched in huttonite or cheralite molecules; (b) LREE versus Pb + Th + U
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The composition of high-Y monazite-(Ce) from sample Fi-9/03 expressed in mo...
Published: 01 April 2010
F ig . 6. The composition of high-Y monazite-(Ce) from sample Fi-9/03 expressed in mol.% monazite, xenotime (Xno), cheralite (Che) and huttonite (Hut).
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The frequently used, but now discredited, six-fold division of  Bowie &amp;...
Published: 01 June 2007
F ig . 1. The frequently used, but now discredited, six-fold division of Bowie & Horne (1953) . After Rose (1980) . A marks the type cheralite, and B, the now-discredited type “brabantite”.