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davidite

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Journal Article
Published: 01 January 2013
American Mineralogist (2013) 98 (1): 275–278.
...Gregory R. Lumpkin; Mark G. Blackford; Michael Colella Abstract Davidite (A 1−x M 21 O 38 ) samples from five different geological localities contain approximately 0.2 to 9.5 wt% UO 2 (0.02 to 0.65 atoms per formula unit) and <0.1 to 1.3 wt% ThO 2 (<0.01 to 0.09 atoms per formula unit...
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Journal Article
Published: 01 November 2007
American Mineralogist (2007) 92 (11-12): 1925–1935.
...Don Chipley; Paul A. Polito; T. Kurtis Kyser Abstract Laser-ablation high-resolution inductively coupled plasma mass spectrometry (LA-HR-ICP-MS) is a rapid, accurate, and inexpensive technique for making in situ U-Pb isotopic measurements of uraninite and davidite. The advantages of this method...
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Journal Article
Published: 01 August 1985
The Canadian Mineralogist (1985) 23 (3): 495–500.
Journal Article
Published: 01 October 1979
American Mineralogist (1979) 64 (9-10): 1010–1017.
...B. M. Gatehouse; I. E. Grey; P. R. Kelly Abstract Davidite from the Pandora Prospect, Pima County, Arizona, crystallizes in the space group R 3 with lattice parameters a = 9.190(3)A, α = 68.73(1)°. Its formula, determined from microprobe analysis, is REE 0.91 U 0.33 Ca 0.20 Y 0.25 (Sr,Th,Pb) 0.09...
Journal Article
Published: 01 June 1968
American Mineralogist (1968) 53 (5-6): 869–879.
.... The structure is based on oxygen closest-packing with, by analogy to the magnetoplumbite structure, Pb in the anion framework. Davidite, which has a unit cell of the same dimensions as that of senaite, has the probable primitive unit cell contents (Ti, Fe, …) 21 O 39 . Copyright © 1968 by the Mineralogical...
Journal Article
Published: 01 June 1961
American Mineralogist (1961) 46 (5-6): 700–718.
...A. Pabst Abstract Partly or wholly metamict davidite from Pima County, Arizona and from Iveland, Norway, has been reconstituted to single crystals or twins by heating in air. The cell dimensions are a 0 10.37 ± 0.02, c 0 20.87 ± 0.02 Å. The space group is R 3 or R 3. The suggested ideal content...
Journal Article
Journal: Economic Geology
Published: 01 March 1961
Economic Geology (1961) 56 (2): 442–444.
...J. D. Hayton Abstract Reply to a paper by J.D. Hayton (GeoScience Abstracts 2-3024). In addition to showing a peculiar and diagnostic lanthanon distribution, davidites are chemically characterized by 1) a relatively high Sr/Ca ratio combined with a low alkaline earth content, 2) a relatively high U...
Journal Article
Journal: Economic Geology
Published: 01 November 1960
Economic Geology (1960) 55 (7): 1541–1550.
...J. R. Butler; R. Hall Abstract "Twelve davidites from several localities and of different parageneses have been analysed for U and individual rare earths. The abundance of the total lanthanons invariably exceeds that of Yt and the distribution of the individual lanthanons is strikingly similar...
Journal Article
Journal: Economic Geology
Published: 01 August 1960
Economic Geology (1960) 55 (5): 1030–1038.
...J. D. Hayton Abstract Rather than a heterogeneous mixture of rutile with one or more radioactive constituents, as suggested by A. W. G. Whittle, davidite is considered a homogeneous mineral in which uranium and the lanthanons are isomorphously replaceable, as well as probably Ti, V, Cr, and Al...
Journal Article
Journal: Economic Geology
Published: 01 January 1959
Economic Geology (1959) 54 (1): 64–81.
...Alick W. G. Whittle Abstract The Precambrian rocks of Australia contain a wider variety of davidites than has been found elsewhere in the world. Investigation of davidite occurrences as an economic U ore over a number of years has revealed its many peculiar physical and chemical characteristics...
Journal Article
Published: 01 August 1951
American Mineralogist (1951) 36 (7-8): 563–572.
... to the davidite from Olary, South Australia, as described by Mawson. The principal metallic elements in the Mozambique mineral are titanium, iron, uranium and chromium. Experimental data further confirm Mawson's original description of davidite as a distinct mineral species. The application of differential...
Journal Article
Journal: Economic Geology
Published: 01 March 1957
Economic Geology (1957) 52 (2): 140–148.
...L. J. Lawrence Abstract "The davidites, which occur disseminated in Archaean schists and granulites, exhibit a number of interesting microtextures and show a wide variation in U 3 O 8 content. In one instance the uranium content appears to be shared between davidite and ilmenite with which...
Image
Different types of veins in albitite associated with davidite in the drilled core samples (a) fracture filling davidite in brick red albitite; (b-c) magnified image of vein-davidite; (d) calcite vein containing davidite crystal in light pink albitite; (e) davidite with calcite and calcite+quartz veins in brick red albitite; (f) calcite+rutile vein in brick red albitite; (g) calcite vein containing davidite and rutile; (h) coarse davidite creating radiation cracks in surrounding calcite.
Published: 01 August 2022
Fig 6. Different types of veins in albitite associated with davidite in the drilled core samples (a) fracture filling davidite in brick red albitite; (b-c) magnified image of vein-davidite; (d) calcite vein containing davidite crystal in light pink albitite; (e) davidite with calcite
Image
(a) Uraninite relicts, RL,1N; (b) fine disseminated uraninite, TL,1N; (c) anhedral davidite in deformed albitite, TL, 2N; (d) subhedral davidite with calcite vein in albitie, TL,1N; (e) euhedral davidite, TL,1N; (f) partly metamict davidite in calcite vein, TL, 1N; (g) bastnaesite rim around metamict davidite within calcite vein, RL,1N; (h) davidite enclosing fine rutile, RL,1N; (i) rutile-hematite intergrowth, RL,1N.
Published: 01 August 2022
Fig 4. (a) Uraninite relicts, RL,1N; (b) fine disseminated uraninite, TL,1N; (c) anhedral davidite in deformed albitite, TL, 2N; (d) subhedral davidite with calcite vein in albitie, TL,1N; (e) euhedral davidite, TL,1N; (f) partly metamict davidite in calcite vein, TL, 1N; (g
Image
(a) Euhedral davidite within rutile-hematite intergrown mass, TL,1N; (b) davidite bearing calcite-quartz vein, TL, 2N; (c) primasatic davidite and corresponding alpha tracks in calcite-quartz vein, TL,1N.
Published: 01 August 2022
Fig. 7. (a) Euhedral davidite within rutile-hematite intergrown mass, TL,1N; (b) davidite bearing calcite-quartz vein, TL, 2N; (c) primasatic davidite and corresponding alpha tracks in calcite-quartz vein, TL,1N.
Image
Representative SEM (backscattered electron) images. (a) Crystalline to partially damaged davidite sample D3 from Connecticut (275 Ma) showing patchy chemical zoning. The origin of the blocky fracture pattern is unknown. Width of image = 3 mm. (b) Weakly zoned, fully amorphous davidite sample D8 from Mozambique (~600 Ma). Width of image = 6 mm. (c) Fully amorphous davidite sample D2 from Norway (295 Ma). Width of image = 5 mm. (d) Fully amorphous davidite sample D4 from Arizona (~150 Ma) showing distinct alteration rim to titanite and minor rutile. Width of image = 4 mm. (e–f). Fully amorphous davidite samples D6 (e) and D7 (f) from Australia (1520 Ma) showing various levels of alteration to ilmenite and rutile. Width of images = 8 mm (e) and 5 mm (f).
Published: 01 January 2013
Figure 1 Representative SEM (backscattered electron) images. ( a ) Crystalline to partially damaged davidite sample D3 from Connecticut (275 Ma) showing patchy chemical zoning. The origin of the blocky fracture pattern is unknown. Width of image = 3 mm. ( b ) Weakly zoned, fully amorphous
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Chondrite-normalized REE patterns for davidite-(La). Normalizing factors from Sun and McDonough (1989). Source data from Table 3.
Published: 01 October 2015
F ig . 7. Chondrite-normalized REE patterns for davidite-(La). Normalizing factors from Sun and McDonough ( 1989 ). Source data from Table 3 .
Image
Backscattered electron images showing alteration of davidite to new phase assemblages. (a) Fully amorphous davidite (white) from Pima County, Arizona, USA replaced by titanite (medium grey) + minor rutile (darker grey). Width of image = 5 mm. (b) Fully amorphous davidite (lighter grey) from Crocker's Well, South Australia, showing alteration to ilmenite (medium grey) + rutile (black), with small inclusions of thorite (white). Width of image = 1 mm.
Published: 01 October 2014
F ig . 6. Backscattered electron images showing alteration of davidite to new phase assemblages. ( a ) Fully amorphous davidite (white) from Pima County, Arizona, USA replaced by titanite (medium grey) + minor rutile (darker grey). Width of image = 5 mm. ( b ) Fully amorphous davidite (lighter
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TEM results. (a–c) Electron diffraction patterns of davidite sample D3 with variable α decay dose values of ~0.2, 0.3, and 0.5 × 1016 α/mg, respectively, showing the appearance of diffuse rings with increasing dose (note, this is also a function of tilt conditions and lattice orientation). (d) Diffraction pattern of fully amorphous davidite D2 showing diffuse rings and no Bragg beams. (e) HRTEM image corresponding to diffraction pattern in b, showing mottled contrast due to amorphous domains in a crystalline matrix. Width of image is ~40 nm.
Published: 01 January 2013
Figure 2 TEM results. ( a – c ) Electron diffraction patterns of davidite sample D3 with variable α decay dose values of ~0.2, 0.3, and 0.5 × 10 16 α/mg, respectively, showing the appearance of diffuse rings with increasing dose (note, this is also a function of tilt conditions and lattice
Image
Backscattered electron images of titanite. (a) Sample SC1 shows clear zoning and extensive fracturing throughout the grain. Nb-rich rutile and chernovite-(Y) are present inside quartz-filled fractures (black contrast). (b) Sample SC2 shows titanite breaking down into secondary phases, including calcite, niobian rutile, davidite-(Ce), and quartz. Abbreviations: cal = calcite; chv = chernovite-(Y); dvd = davidite-(Ce); Nb-rt = niobian rutile; ttn = titanite. (Color online.)
Published: 01 April 2025
phases, including calcite, niobian rutile, davidite-(Ce), and quartz. Abbreviations: cal = calcite; chv = chernovite-(Y); dvd = davidite-(Ce); Nb-rt = niobian rutile; ttn = titanite. (Color online.)