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brazilianite

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Journal Article
Published: 01 August 2013
American Mineralogist (2013) 98 (8-9): 1624–1630.
...G. Diego Gatta; Pietro Vignola; Martin Meven; Romano Rinaldi Abstract The chemical composition and the crystal structure of a gem-quality brazilianite from the Telírio pegmatite, near Linópolis, Minas Gerais, Brazil, [NaAl 3 (PO 4 ) 2 (OH) 4 , a = 11.2448(5) Å, b = 10.1539(6) Å, c = 7.1031(3) Å, β...
FIGURES
Journal Article
Published: 01 December 2000
Mineralogical Magazine (2000) 64 (6): 1147–1164.
... mineral natromontebrasite NaAl(PO 4 )(OH,F) is reported from the Daheim pegmatite. In the Okatjimukuju pegmatite, montebrasite has been replaced by a number of phases including crandallite CaAl 3 (PO 4 ) 2 (OH) 5 ·H 2 O and brazilianite NaAl 3 (PO 4 ) 2 (OH) 4 . In one example, montebrasite has been...
FIGURES | View All (6)
Journal Article
Published: 01 April 1948
American Mineralogist (1948) 33 (3-4): 135–144.
...Clifford Frondel; Marie Louise Lindberg Abstract Brazilianite occurs in the Palermo pegmatite, North Groton, Grafton County, New Hampshire. It differs in crystal habit from that of the crystals from Brazil. Chemical analysis confirms the formula NaAl 3 (PO 4 ) 2 (OH) 4 . X -ray data...
Journal Article
Published: 01 October 1946
American Mineralogist (1946) 31 (9-10): 507.
...Cornelius S. Hurlbut, Jr.; Elizabeth J. Weichel Abstract Brazilianite, the new phosphate, Na 2 Al 6 P 4 O 16 (OH) 8 , is described by Pough and Henderson * as follows: monoclinic, β = 97°22′, perfect {010} cleavage; specific gravity 2.94; axial ratios a:b:c = 1.1056:1:0.6992. Copyright © 1946...
Journal Article
Published: 01 October 1945
American Mineralogist (1945) 30 (9-10): 572–582.
...Frederick H. Pough; Edward P. Henderson Abstract Brazilianite is a new monoclinic phosphate mineral, Na 2 Al 6 P 4 O 16 (OH) 8 . a:b:c = 1.1056: 1:0.6992; β=97°22', p 0 ' = 0.6377, q 0 ' = 0.6992, x'=0.1293. Perfect (010) cleavage. H = 5½, S.G. = 2.94, vitreous luster, yellow-green, translucent...
Image
(a) Crystal of brazilianite. The white areas are the original montebrasite (M) which has been almost entirely replaced by dark grey brazilianite (B). Length of crystal = 2.5 cm. (b) Backscattered electron image of quartz (Q) (grey), fluorapatite (F) (white) and brazilianite (black) intergrown with apatite (white) from the Okatjimukuju pegmatite, Karibib. Scale bar = 500 μm. (c) A magnification of a section of part b showing the brazilianite (black) apatite (white) intergrowth and including a magnesium aluminium phosphate mineral (lazulite). Scale bar = 100 μm. (d) Backscattered electron image of brazilianite (B) with montebrasite (M) remnants. Scale bar = 100 μm. (e) Backscattered electron image of a zoned crystal of apatite, with a Sr-rich goyazite centre, in brazilianite. Scale bar: 100 μm.
Published: 01 December 2000
F ig . 3. ( a ) Crystal of brazilianite. The white areas are the original montebrasite (M) which has been almost entirely replaced by dark grey brazilianite (B). Length of crystal = 2.5 cm. ( b ) Backscattered electron image of quartz (Q) (grey), fluorapatite (F) (white) and brazilianite (black
Image
The crystal structures of petersite-(Y) and brazilianite: (a) petersite-(Y) projected onto (001); (b) petersite-(Y) projected onto (010); (Cu2+ϕ6) octahedra are shadow-shaded, Y is shown as shaded circles; (c) brazilianite projected onto (001); (d) brazilianite projected onto (010); (Alϕ6) octahedra are shadow-shaded, Na is shown as shaded circles.
Published: 01 January 2002
Figure 40. The crystal structures of petersite-(Y) and brazilianite: (a) petersite-(Y) projected onto (001); (b) petersite-(Y) projected onto (010); (Cu 2+ ϕ 6 ) octahedra are shadow-shaded, Y is shown as shaded circles; (c) brazilianite projected onto (001); (d) brazilianite projected onto (010
Image
Optical photomicrographs from the Al-rich phosphatic nodules from the Buranga pegmatite. (a) Anhedral wyllieite crystal surrounded by brazilianite and quartz. Plane polarizers. (b) Anhedral and fractured montebrasite crystal surrounded by coarse-grained brazilianite and quartz. Plane polarizers. (c) Partially resorbed trolleite crystal enclosed by euhedral quartz and brazilianite. Crossed polarizers. (d) Subhedral trolleite surrounded by interstitial scorzalite and euhedral quartz. Note primary fluid inclusions aligned in growth zones of trolleite, and the mixture of fluid, melt, and crystal inclusions in the quartz grain on the top right (dotted lines). Plane polarizers. (e) Pseudomorph after rosemaryite partially replaced by a combination of eosphorite and samuelsonite. Bertossaite partially rims the bottom part of the pseudomorph. Scorzalite grows in the contacts with trolleite. Gypsum plate inserted. (f) Euhedral radiating crystals of burangaite replacing trolleite. Plane polarizers. Mineral abbreviations: Brz = brazilianite; Bts = bertossaite; Bur = burangaite; Eo = eosphorite; Mbs = montebrasite; Qz = quartz; Rsm = rosemaryite; Scz = scorzalite; Sm = samuelsonite; Trl = trolleite; Wyl = wyllieite. (Color online.)
Published: 01 February 2023
Figure 5. Optical photomicrographs from the Al-rich phosphatic nodules from the Buranga pegmatite. ( a ) Anhedral wyllieite crystal surrounded by brazilianite and quartz. Plane polarizers. ( b ) Anhedral and fractured montebrasite crystal surrounded by coarse-grained brazilianite and quartz
Image
Two views of the crystal structure of brazilianite (i.e., down [100] and [001]) based on the neutron structure refinement of this study. Thermal ellipsoid probability factor: 60%. Al-octahedra are in light gray, P-tetrahedra in dark gray, Na sites (medium gray) as un-bonded atoms, H sites in white.
Published: 01 August 2013
Figure 1 Two views of the crystal structure of brazilianite (i.e., down [100] and [001]) based on the neutron structure refinement of this study. Thermal ellipsoid probability factor: 60%. Al-octahedra are in light gray, P-tetrahedra in dark gray, Na sites (medium gray) as un-bonded atoms, H
Journal Article
Published: 01 February 1955
American Mineralogist (1955) 40 (1-2): 50–63.
.... Hydrothermal and other alteration has formed brazilianite (a second Brazilian occurrence for this mineral), crandallite, wardite and apatite, from the amblygonite. Eosphorite, hureaulite, metastrengite, stewartite, ferri-sicklerite, heterosite, rockbridgeite(?), and a number of unidentified minerals, have been...
Image
Hand samples from the Buranga pegmatite examined in this study. (a) Sample BU19 (RGM9705, in the notation of the Royal Museum for Central Africa), partially altered phosphatic nodule dominated by trolleite (light blue) with altered crystals of rosemaryite (brownish) and scattered scorzalite (dark blue). The right part of the sample is composed of secondary brazilianite (cream-colored to white). The concentric diagonal curves, especially visible at the bottom left of the sample, are saw scratches. (b) Sample BU04 (RGM9696), strongly altered phosphatic nodule composed of bertossaite (pinkish cream), trolleite (light blue), brazilianite (white cream), and scorzalite (dark blue spots). (c) Sample BU24 (RGM8894), albitized facies, composed mainly of albite (cream-colored) with oxidation spots (reddish spots) and few tourmaline crystals (black spots). (Color online.)
Published: 01 February 2023
scorzalite (dark blue). The right part of the sample is composed of secondary brazilianite (cream-colored to white). The concentric diagonal curves, especially visible at the bottom left of the sample, are saw scratches. ( b ) Sample BU04 (RGM9696), strongly altered phosphatic nodule composed of bertossaite
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Hydrogen sites location, H-bonding scheme, and configuration of the Na-polyhedron in the structure of brazilianite based on the neutron structure refinement of this study. The sites H(2a) and H(2b) are mutually exclusive. Thermal ellipsoid probability factor: 60%.
Published: 01 August 2013
Figure 2 Hydrogen sites location, H-bonding scheme, and configuration of the Na-polyhedron in the structure of brazilianite based on the neutron structure refinement of this study. The sites H(2a) and H(2b) are mutually exclusive. Thermal ellipsoid probability factor: 60%.
Journal Article
Published: 01 September 2005
European Journal of Mineralogy (2005) 17 (5): 749–759.
... 3 mm, embedded in scorzalite. Associated phosphate minerals are scorzalite, trolleite, montebrasite, bertossaite, brazilianite, with accessory augelite, triplite and lacroixite. The mineral is transparent and exhibits a dark-green to bronze colour, with a resinous lustre and with a greenish...
FIGURES | View All (7)
Journal Article
Published: 01 October 1999
American Mineralogist (1999) 84 (10): 1674–1679.
... feldspar, muscovite, beryl, columbite, possibly heterosite, and powdery coatings of Mn- and Fe-oxides; in the dumps of the pegmatite, there are numerous other phosphates including altered triphylite-lithophyllite, arrojadite, eosphorite, laueite, brazilianite, and fairfieldite. Bederite is very dark brown...
Journal Article
Published: 01 February 1982
American Mineralogist (1982) 67 (1-2): 97–113.
... is the result of subsolidus reactions with residual pegmatitic fluids. Spodumene has been replaced by eucryptite, albite, and micas. Alteration products of montebrasite include low-fluorine secondary montebrasite, crandallite (tentative), hydroxylapatite, muscovite, brazilianite, augelite (tentative...
Journal Article
Published: 01 February 2023
American Mineralogist (2023) 108 (2): 277–296.
...Figure 5. Optical photomicrographs from the Al-rich phosphatic nodules from the Buranga pegmatite. ( a ) Anhedral wyllieite crystal surrounded by brazilianite and quartz. Plane polarizers. ( b ) Anhedral and fractured montebrasite crystal surrounded by coarse-grained brazilianite and quartz...
FIGURES | View All (17)
Journal Article
Published: 01 August 1953
American Mineralogist (1953) 38 (7-8): 728–729.
... that occur at the locality include hurlbutite, tiny beryl-lonite crystals, small twinned crystals of amblygonite and brazilianite as small single crystals and as aggregates of parallely intergrown crystals up to an inch in length. Copyright © 1953 by the Mineralogical Society of America 1953...
Journal Article
Published: 01 February 1949
American Mineralogist (1949) 34 (1-2): 83–93.
... include albite, muscovite, quartz, scorzalite (new mineral), souzalite (new mineral), brazilianite, apatite, zircon, tapiolite, and two unidentified phosphate minerals. Detailed descriptions, with chemical analyses, are given for scorzalite and souzalite, both of which are hydrous iron magnesium aluminum...
Journal Article
Published: 30 September 2019
The Canadian Mineralogist (2019) 57 (5): 733–734.
..., jahnsite group species, mitridatite, pseudolaueite, laueite and stewartite. Accessory montebrasite, fairfieldite, eosphorite–childrenite, kastningite, brazilianite, and goyazite also occur. In particular, montebrasite that appears gray is rich in goyazite, fluorapatite, albite and muscovite appear...
Image
Mixed Fe-Nb-Ta-rich rutile and CGM grain. (a) BSE image of the mapped area. The chemical formulas of analyses 1–3 marked on the image are provided. (b to f) CLS maps of the assemblage. Raman image was acquired in a 2 × 2 µm regular array with a 532 nm laser, 150 g/mm grating, 25% laser power, 50× long working distance objective, 30 µm confocal pinhole, single accumulation of 0.2 s, and detector EM gain of 500. (b) Combined maps showing the spatial distributions of each phase. (c) Trolleite/brazilianite phase map. (d) CGM phase map. (e) Rutile phase map. (f) Trolleite phase map. (Color online.)
Published: 01 February 2023
% laser power, 50× long working distance objective, 30 µm confocal pinhole, single accumulation of 0.2 s, and detector EM gain of 500. ( b ) Combined maps showing the spatial distributions of each phase. ( c ) Trolleite/brazilianite phase map. ( d ) CGM phase map. ( e ) Rutile phase map. ( f ) Trolleite