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childrenite

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Journal Article
Published: 01 August 1958
American Mineralogist (1958) 43 (7-8): 765–768.
...Horace Winchell Abstract Hurlbut (1950) discussed the evidence that the childrenite-eosphorite series Mn 1– x Fe x Al(PO 4 )(OH) 2 (H 2 O) is indeed a continuous isomorphous series, citing examples with x = 0.04, 0.14, 0.16, 0.23, 0.32, 0.33, 0.39, 0.47, 0.85, and 0.91, and giving in summary...
Journal Article
Published: 01 June 1951
American Mineralogist (1951) 36 (5-6): 509–511.
...W. H. Barnes; Violet C. Shore Abstract On the basis of an exhaustive optical study of the childrenite-eosphorite series, Professor C. S. Hurlbut ( Am. Mineral. , 35 , 793–805, 1950) concludes that these minerals should be classified in the monoclinic system. Previous morphological ( Dana's Textbook...
Journal Article
Published: 01 October 1950
American Mineralogist (1950) 35 (9-10): 793–805.
...Cornelius S. Hurlbut, Jr. Abstract An optical study of the childrenite-eosphorite series shows twinning in all well-crystallized members indicating monoclinic symmetry. In singly terminated crystals twinning is on {100}; in doubly terminated crystals twinning is on both {100} and {001...
Journal Article
Published: 01 February 1949
American Mineralogist (1949) 34 (1-2): 12–18.
...William H. Barnes Abstract The unit cell constants and the space group of childrenite, AlPO 4 · Fe(OH) 2 · 2H 2 O, have been determined by the Buerger precession method with the following results: a = 10.38 Å, b = 13.36 Å c = 6.911 Å a:b:c =0.7766:1:0.5173; Z = 8; calculated density = 3.186 g./cc...
Image
The crystal structures of childrenite and jahnsite: (a) childrenite projected onto (100); (b) childrenite projected onto (001); (Alϕ6) octahedra are shadow-shaded, Mn2+ cations are shown as circles; (c) jahnsite projected onto (001); (d) jahnsite projected onto (010); (Fe3+ϕ6) octahedra are 44-net-shaded, Ca atoms are shown as circles, (Mn2+ϕ6) and (Mgϕ6) octahedra are shadow-shaded.
Published: 01 January 2002
Figure 20. The crystal structures of childrenite and jahnsite: (a) childrenite projected onto (100); (b) childrenite projected onto (001); (Alϕ 6 ) octahedra are shadow-shaded, Mn 2+ cations are shown as circles; (c) jahnsite projected onto (001); (d) jahnsite projected onto (010); (Fe 3+ ϕ 6
Image
Published: 28 January 2021
TABLE 7. SELECTED MICROPROBE COMPOSITIONS OF THE EOSPHORITE–CHILDRENITE SERIES AND WHITEITE GROUP MINERALS
Image
Prismatic crystal of natropalermoite growing on greyish brown childrenite. Note weak striations parallel to the axis of elongation a. The top portion of this crystal was used for X-ray, chemistry and optical data collection.
Published: 01 August 2017
Fig. 2. Prismatic crystal of natropalermoite growing on greyish brown childrenite. Note weak striations parallel to the axis of elongation a . The top portion of this crystal was used for X-ray, chemistry and optical data collection.
Image
Microphotographs of (a) ferrisicklerite (Fsk) displaying a red-brownish color, locally altered to the eosphorite–childrenite (Eos-Chi) series; (b) reddish ferrisicklerite nearly fully replaced by yellowish jahnsite-(CaMnFe) (Jhn), opaque lipscombite and/or barbosalite (Lcb/Bbs), orange eosphorite–childrenite (Eos-Chi), brownish-greenish rockbridgeite (Rck), and subrounded dark crystals of an unidentified phosphate (TARP1), which resembles cacoxenite; (c) very fine grained spherulitic aggregates of strongly pleochroic greenish rockbridgeite (Rck) growing among silicates; (d) pale yellowish acicular jahnsite-(CaMnFe) (Jhn) partly replaced by lipscombite and/or barbosalite (Lcb/Bbs); (e) eosphorite–childrenite (Eos-Chi) subhedral crystal showing some darker (orange) areas along the rim, including a small, black, rounded unidentified phosphate (TARP1) crystal; and (f) a cluster of whiteite group minerals (Whi) radially disposed in cross-polarized light.
Published: 28 January 2021
Fig. 2. Microphotographs of (a) ferrisicklerite (Fsk) displaying a red-brownish color, locally altered to the eosphorite–childrenite (Eos-Chi) series; (b) reddish ferrisicklerite nearly fully replaced by yellowish jahnsite-(CaMnFe) (Jhn), opaque lipscombite and/or barbosalite (Lcb/Bbs), orange
Journal Article
Published: 01 December 1975
American Mineralogist (1975) 60 (11-12): 957–964.
... quartz, siderite, scorzalite, goyazite, palermoite, bjarebyite, childrenite, arrojadite, and many very late products. Foggite , Ca(H 2 O)Al(OH) 2 [P0 4 ], a 9.270(2)Å, b 21.324(7)Å, c 5.190(2)Å, A 2 1 22, Z = 8, specific gravity 2.78, hardness 4, cleavages {010} perfect and {100} good, occurs...
Journal Article
Published: 01 October 2008
The Canadian Mineralogist (2008) 46 (5): 1131–1157.
... (apatite manganifère, monazite) dans l’aplite THM est contemporaine d’un événement thermique à environ 302 Ma suivant la mise en place du granite post-kinématique de Flossenbürg. Les séquences 1a et 1b, contenant les solutions solides lazulite et childrenite–éosphorite et la gordonite, sont...
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Micromorphological changes and chemical variation of rockbridgeite. a) Colloform rhythmites in quartz – muscovite (mu) – biotite (bt) matrix. The transect of the line scan is shown by a double line (BSE image). b) Variation of FeO, P2O5, Al2O3, MnO and Na2O along a transect through phosphate crusts revealing gradual changes from rockbridgeite, through Al-bearing rockbridgeite into a hydrated form of Fe–Al phosphate (most likely an intergrowth of rockbridgeite or “ferrolaueite” or both and childrenite). This zonal arrangement of mineralization shows how exo-aplitic (childrenite) and intra-aplitic sequences (rockbridgeite) correspond with each other.
Published: 01 October 2008
through phosphate crusts revealing gradual changes from rockbridgeite, through Al-bearing rockbridgeite into a hydrated form of Fe–Al phosphate (most likely an intergrowth of rockbridgeite or “ferrolaueite” or both and childrenite). This zonal arrangement of mineralization shows how exo-aplitic
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Selected chains from phosphate structures; (a) bøggildite; (b) collinsite; (c) childrenite; (d) tancoite; (e) bearthite. Legend as in Fig. 24.
Published: 01 August 2014
F ig . 25. Selected chains from phosphate structures; ( a ) bøggildite; ( b ) collinsite; ( c ) childrenite; ( d ) tancoite; ( e ) bearthite. Legend as in Fig. 24 .
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Comparison of high resolution Fe 2p3/2 XPS spectrum of ferroberaunite with patterns of ferric (beraunite/‘eleonorite’) and ferrous phosphates (vivianite and childrenite). The spectra are vertically shifted. The numbering of peaks corresponds to Table 2; the peaks Fe2p3/2(1) used to estimate a relative content of Fe2+ are highlighted.
Published: 16 February 2022
Fig. 5. Comparison of high resolution Fe 2p 3/2 XPS spectrum of ferroberaunite with patterns of ferric (beraunite/‘eleonorite’) and ferrous phosphates (vivianite and childrenite). The spectra are vertically shifted. The numbering of peaks corresponds to Table 2 ; the peaks Fe2p 3/2 (1) used
Journal Article
Published: 08 January 2021
The Canadian Mineralogist (2020) 58 (6): 733–746.
... of triphylite by ferrisicklerite and heterosite; and (3) hydrothermal, with secondary growth of alluaudite at the expense of heterosite and wardite from montebrasite caused by Na-metasomatism. A Ca-rich influx under oxidizing conditions produced childrenite–eosphorite–ernstite, jahnsite-(CaMnFe...
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BSE images of secondary phosphates: (a) acicular rockbridgeite, mitridatite, childrenite and secondary apatite replacing a primary quartz (Qz)-muscovite (Mus)-biotite (Bt) assemblage. (b) Collomorphous rockbridgeite with relics of muscovite (Mus) and biotite (Bt). Inset: element variations along a microprobe traverse in the Fe-rich phosphate.
Published: 01 June 2006
F ig . 4. BSE images of secondary phosphates: ( a ) acicular rockbridgeite, mitridatite, childrenite and secondary apatite replacing a primary quartz (Qz)-muscovite (Mus)-biotite (Bt) assemblage. ( b ) Collomorphous rockbridgeite with relics of muscovite (Mus) and biotite (Bt). Inset: element
Journal Article
Published: 26 June 2017
European Journal of Mineralogy (2017) 29 (5): 923–930.
... granitic pegmatite, Minas Gerais, Brazil. It occurs as tiny dodecahedral {1 1 0} crystals, deposited on moraesite fibres. Associated primary minerals are albite, montebrasite, Li-bearing micas, cassiterite, elbaite and quartz, while the secondary phosphate association contains fluorapatite, childrenite...
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Journal Article
Published: 01 May 2017
The Canadian Mineralogist (2017) 55 (3): 377–397.
... inclusions show a main mineralogy composed of muscovite, α-quartz, mogánite, dickite, and minor feldspars which demonstrate, in combination with the observation of dawsonite, nahcolite, jeremejevite, and childrenite daughter minerals, a CO 2 -, H 2 O-, B 2 O 3 -, and P 3 O 4 -enriched peraluminous boro...
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Journal Article
Published: 01 April 2017
American Mineralogist (2017) 102 (4): 728–742.
... origin for the graphite. The Belvís pluton is a reversely zoned massif composed by four highly fractionated granite units, showing a varied accessory phosphate phases: U-rich monazite, U-rich xenotime, U-rich fluorapatite, and late eosphorite-childrenite. The strong peraluminous character of the granites...
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Journal Article
Published: 01 February 2012
Mineralogical Magazine (2012) 76 (1): 1–24.
... and triplite, and altered the granites, aplites and pegmatites, replacing some of the phosphate minerals and feldspars and depositing goyazite, montebrasite and childrenite–eosphorite. The interaction of the residual hydrothermal fluids with those from the surrounding metamorphic rocks during later alteration...
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Journal Article
Published: 01 June 2009
Mineralogical Magazine (2009) 73 (3): 415–420.
..., quartz, albite, beryl, amblygonite-montebrasite, childrenite-eosphorite and apatite, and crystallized as one of the latest minerals during pocket formation. It is off-white to pale yellow or light tan, translucent with a white streak and a vitreous lustre, and shows light blue to pale yellow...
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