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1-20 OF 52 RESULTS FOR
farringtonite
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Journal Article
The farringtonite/Mg 3 (PO 4 ) 2 -II transformation; a new curve for pressure calibration in piston-cylinder apparatus
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
Published: 01 April 1996
European Journal of Mineralogy (1996) 8 (2): 349–354.
Journal Article
Cation distribution studies of some ternary orthophosphates having the farringtonite structure
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 June 1985
American Mineralogist (1985) 70 (5-6): 624–629.
...Anders G. Nord; Tore Ericsson Abstract Solid solutions, mainly with the composition (Zn 0.70 Fe 0.25 Me 0.05 ) 3 (PO 4 ) 2 , have been analyzed by 57 Fe Mössbauer spectroscopy (Me = Mg, Mn, Fe, Co, Ni, Cd or Ca). The structure is isomorphous with “ γ -Zn 3 (PO 4 ) 2 ” and with farringtonite (Mg 3...
Journal Article
New X-Ray and Compositional Data for Farringtonite, Mg 3 (PO 4 ) 2
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 October 1973
American Mineralogist (1973) 58 (9-10): 949–951.
...Louis H. Fuchs; Edward Olsen; Elizabeth Gebert Abstract New data for the meteoritic mineral farringtonite indicates that it is essentially Mg 3 (PO 4 ) 2 with some Fe 2+ substitution for Mg but with less than 0.05 wt percent Si substitution for P. Farringtonite has a = 8.79, b = 8.22, c = 5.07 Å β...
Image
The crystal structures of farringtonite and beusite: (a) farringtonite proj...
Published: 01 January 2002
Figure 46. The crystal structures of farringtonite and beusite: (a) farringtonite projected onto (001); (b) farringtonite projected onto (010); (MgO 6 ) octahedra are shadow-shaded, (MgO 5 ) polyhedra are line-shaded; (c) a layer of the beusite structure projected onto (100); (d) another layer
Journal Article
Chopinite-sarcopside solid solution, [(Mg,Fe) 3 □](PO 4 ) 2 , in GRA95209, a transitional acapulcoite: Implications for phosphate genesis in meteorites
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 February 2010
American Mineralogist (2010) 95 (2-3): 260–272.
... backscatter diffraction patterns and maps, together with chemical analyses and Fe-Mg-Mn distribution among phosphates, confirm identification of the orthophosphate as sarcopside, chopinite, and farringtonite; no graftonite was found. Phosphates are found as (1) narrow rims between metal and forsterite...
Image
Back-scattered electron (BSE) images of fayalitic rims on forsterite in GRA...
in Chopinite-sarcopside solid solution, [(Mg,Fe) 3 □](PO 4 ) 2 , in GRA95209, a transitional acapulcoite: Implications for phosphate genesis in meteorites
> American Mineralogist
Published: 01 February 2010
exposed by fragmentation of the section. ( b ) Contrast-enhanced, brightened, and enlarged portion of BSE image enclosed in white frame in a to bring out M-shaped area of farringtonite (Table 6 ). ( c ) Map of the M-shaped area of farringtonite obtained by electron backscatter diffraction (Table 1
Image
Compositions (mole proportions) of (Mg,Fe,Mn) 3 (PO 4 ) 2 phases analyzed ...
in Chopinite-sarcopside solid solution, [(Mg,Fe) 3 □](PO 4 ) 2 , in GRA95209, a transitional acapulcoite: Implications for phosphate genesis in meteorites
> American Mineralogist
Published: 01 February 2010
in composition to grains so characterized. However, the identity of one composition (queried farringtonite) is richer in Fe than other farringtonite. Data for type chopinite and terrestrial compositions are from Grew et al. (2007) supplemented by analyses of sarcopside and graftonite in a sample from the Bull
Image
BSE images. Springwater contains abundant phosphoran olivine (shaded in red...
in Phosphoran olivine overgrowths: Implications for multiple impacts to the Main Group pallasite parent body
> American Mineralogist
Published: 01 October 2015
of farringtonite in matrix ( a ) with predominantly metal matrix ( b ). Phases indicated are olivine (ol), taenite and kamacite (Fe-Ni), farringtonite (far), troilite (tro), stanfieldite (sta), and schreibersite (scb). (Locations marked 2a, 2b, and 2c correspond to Fig. 2 .)
Image
( a ) Variation of Mn/Fe ratio with X Mg = Mg/(Mg+Fe) ratio in chladniit...
in Chopinite-sarcopside solid solution, [(Mg,Fe) 3 □](PO 4 ) 2 , in GRA95209, a transitional acapulcoite: Implications for phosphate genesis in meteorites
> American Mineralogist
Published: 01 February 2010
(e.g., Fig. 6b ). The identity of one composition (queried farringtonite) is richer in Fe than other farringtonite. Sources of data: Floss (1999) ; T. McCoy (personal communication 2005); McCoy et al. (2006) ; this study.
Image
Thermal expansion of MgAlPO 4 O and farringtonite at 0.1 Mpa.
in Polymorphism and thermochemistry of MgAlPO 4 O, a product of lazulite breakdown at high temperature
> European Journal of Mineralogy
Published: 01 March 2007
Fig. 6. Thermal expansion of MgAlPO 4 O and farringtonite at 0.1 Mpa.
Image
Compressibility of α′-MgAlPO 4 O and farringtonite, Mg 3 (PO 4 ) 2 , at roo...
in Polymorphism and thermochemistry of MgAlPO 4 O, a product of lazulite breakdown at high temperature
> European Journal of Mineralogy
Published: 01 March 2007
Fig. 8. Compressibility of α′-MgAlPO 4 O and farringtonite, Mg 3 (PO 4 ) 2 , at room temperature (MAX80 data).
Image
Maximum binary ranges in mol% Fe 3 (PO 4 ) 2 and Mn 3 (PO 4 ) 2 for compo...
in Chopinite-sarcopside solid solution, [(Mg,Fe) 3 □](PO 4 ) 2 , in GRA95209, a transitional acapulcoite: Implications for phosphate genesis in meteorites
> American Mineralogist
Published: 01 February 2010
F igure 1. Maximum binary ranges in mol% Fe 3 (PO 4 ) 2 and Mn 3 (PO 4 ) 2 for compositions of (Mg,Fe,Mn) 3 (PO 4 ) 2 (orthophosphate) structures obtained by synthesis. Farringtonite at 1 bar, 800°C ( Annersten et al. 1980 ; Nord and Stefanidis 1980), Mn-Fe sarcopside at 200–800 bars, 300°C
Image
Thermal expansion of α′-MgAlPO 4 O and farringtonite (Mg 3 (PO 4 ) 2 ) at 1...
in Polymorphism and thermochemistry of MgAlPO 4 O, a product of lazulite breakdown at high temperature
> European Journal of Mineralogy
Published: 01 March 2007
Fig. 7. Thermal expansion of α′-MgAlPO 4 O and farringtonite (Mg 3 (PO 4 ) 2 ) at 1.7(2) GPa (Max80 data).
Journal Article
Polymorphism and thermochemistry of MgAlPO 4 O, a product of lazulite breakdown at high temperature
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
Published: 01 March 2007
European Journal of Mineralogy (2007) 19 (2): 159–172.
...Fig. 6. Thermal expansion of MgAlPO 4 O and farringtonite at 0.1 Mpa. ...
Image
( a ) Percent of overgrowths observed in contact with farringtonite, stanfi...
in Phosphoran olivine overgrowths: Implications for multiple impacts to the Main Group pallasite parent body
> American Mineralogist
Published: 01 October 2015
Figure 3 ( a ) Percent of overgrowths observed in contact with farringtonite, stanfieldite, metal, troilite, and schreibersite, as compared with the expected profile assuming a random distribution of overgrowths (based on the estimated relative abundances of each phase at host olivine grain
Image
Back-scattered electron images of phosphates in GRA95209. ( a ) Chladniite ...
in Chopinite-sarcopside solid solution, [(Mg,Fe) 3 □](PO 4 ) 2 , in GRA95209, a transitional acapulcoite: Implications for phosphate genesis in meteorites
> American Mineralogist
Published: 01 February 2010
F igure 5. Back-scattered electron images of phosphates in GRA95209. ( a ) Chladniite rim between metal and plagioclase plus enstatite, PTS, 39, area 1–8. ( b ) Chladniite and farringtonite in rim near forsterite, PTS, 39, area 5 ( c ) Forsterite with fayalite rim against chladniite
Image
Heat capacity of MgAlPO 4 O and farringtonite, Mg 3 (PO 4 ) 2 , measured in...
in Polymorphism and thermochemistry of MgAlPO 4 O, a product of lazulite breakdown at high temperature
> European Journal of Mineralogy
Published: 01 March 2007
Fig. 5. Heat capacity of MgAlPO 4 O and farringtonite, Mg 3 (PO 4 ) 2 , measured in the interval-scanning mode (DSC, open circles) and using PPMS (triangles). The endothermic peak at 754 K corresponds to the β″- α′ phase transformation of MgAlPO 4 O.
Image
Feasibility region for the reaction 3 MgAlPO 4 O ⇔ farringtonite + β-berlin...
in Polymorphism and thermochemistry of MgAlPO 4 O, a product of lazulite breakdown at high temperature
> European Journal of Mineralogy
Published: 01 March 2007
Fig. 13. Feasibility region for the reaction 3 MgAlPO 4 O ⇔ farringtonite + β-berlinite + corundum. The feasibility region is defined by the elongated polygon between the intersections A, B and C. Inserted diagram: determination of the enthalpy of formation using the PPMS value for the third-law
Image
Plot of natural farringtonite, graftonite, sarcopside, and chopinite compos...
in Chopinite, [(Mg, Fe) 3 □](PO 4 ) 2 , a new mineral isostructural with sarcopside, from a fluorapatite segregation in granulite-facies paragneiss, Larsemann Hills, Prydz Bay, East Antarctica
> European Journal of Mineralogy
Published: 01 March 2007
Fig. 2. Plot of natural farringtonite, graftonite, sarcopside, and chopinite compositions in terms of the divalent cations excluding Ca. The fields for terrestrial graftonite (dashed line) and sarcopside (solid line) are largely from intergrowths ( Černý et al. , 1998 ; Corbella i Cordomí
Image
Stability field of MgAlPO 4 O and results of bracketing experiments of the ...
in Polymorphism and thermochemistry of MgAlPO 4 O, a product of lazulite breakdown at high temperature
> European Journal of Mineralogy
Published: 01 March 2007
Fig. 9. Stability field of MgAlPO 4 O and results of bracketing experiments of the reaction 3 MgAlPO 4 O ⇔ farringtonite + berlinite + corundum. α-β transition of berlinite according to Cohen & Klement (1973) .
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