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copiapite group

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Journal Article
Published: 04 February 2025
The Canadian Journal of Mineralogy and Petrology (2025) 63 (1): 79–89.
...Juraj Majzlan; Edgar Dachs; Artur Benisek Abstract Copiapite-group minerals are common products of weathering of sulfides, especially pyrite and pyrrhotite. They have a general formula A Fe 3+ 4 (SO 4 ) 6 (OH) 2 ·20H 2 O and all crystallize in the triclinic crystal system (space group P...
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Journal Article
Published: 01 October 2007
Mineralogical Magazine (2007) 71 (5): 553–569.
... octahedrally coordinated A sites. Our synthetic and natural copiapite samples can be divided into two large groups based on the orientation of the structural fragments. One group comprises copiapite phases where A = Al 3+ , Fe 2+ or Fe 3+ and we designate it as the structural type AL. The other group consists...
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Journal Article
Published: 01 February 1985
The Canadian Mineralogist (1985) 23 (1): 53–56.
Journal Article
Published: 01 October 1980
American Mineralogist (1980) 65 (9-10): 961–967.
...., by solutions of linear simultaneous equations. Proportions in the X and R positions of the structural formula are assumed 1:4 on the basis of substitution which at the same time serves as a check on obtained solutions. Identified species of the copiapite group include aluminocopiapite, copiapite...
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Published: 04 February 2025
TABLE 1. AMOUNTS OF CHEMICALS USED FOR THE SYNTHESES OF THE COPIAPITE-GROUP PHASES IN THIS WORK
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Heat capacity (Cp) data for the copiapite-group samples. (a) Entire data sets generated by relaxation calorimetry. (b) Low-temperature portion of the data sets, scaled as Cp/T, to demonstrate the upturn of the heat capacity at T < 5 K.
Published: 04 February 2025
Fig. 2. Heat capacity ( C p ) data for the copiapite-group samples. (a) Entire data sets generated by relaxation calorimetry. (b) Low-temperature portion of the data sets, scaled as C p / T , to demonstrate the upturn of the heat capacity at T < 5 K.
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Published: 04 February 2025
TABLE 3. THERMOCHEMICAL CYCLES FOR THE CALCULATION OF THE ENTHALPIES OF FORMATION OF THE COPIAPITE-GROUP PHASES (ΔH 23 THROUGH ΔH 26 )
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(a) The [M(TØ4)3] octahedral–tetrahedral chain in ferrinatrite; (b) the arrangement of [M(TØ)3] chains in ferrinatrite; (c) the [M2(TØ4)3Ø5] chain in the minerals of the copiapite group; (d) the structure of copiapite; (e) the chain in destinezite; (f) packing of the chains in destinezite; (g) the [M(TO4) Ø2] chain in linarite; (h) packing of [M(TO4) Ø2] chains in linarite. (i) the [M(TO4)2Ø] chain in wherryite; (j) packing of [M(TO4)2Ø] chains in wherryite.
Published: 01 January 2000
Figure 23. (a) The [ M ( T Ø 4 ) 3 ] octahedral–tetrahedral chain in ferrinatrite; (b) the arrangement of [ M ( T Ø) 3 ] chains in ferrinatrite; (c) the [ M 2 ( T Ø 4 ) 3 Ø 5 ] chain in the minerals of the copiapite group; (d) the structure of copiapite; (e) the chain in destinezite; (f
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(a) The [M(TØ4)3] octahedral–tetrahedral chain in ferrinatrite; (b) the arrangement of [M(TØ)3] chains in ferrinatrite; (c) the [M2(TØ4)3Ø5] chain in the minerals of the copiapite group; (d) the structure of copiapite; (e) the chain in destinezite; (f) packing of the chains in destinezite; (g) the [M(TO4) Ø2] chain in linarite; (h) packing of [M(TO4) Ø2] chains in linarite. (i) the [M(TO4)2Ø] chain in wherryite; (j) packing of [M(TO4)2Ø] chains in wherryite.
Published: 01 January 2000
Figure 23. (a) The [ M ( T Ø 4 ) 3 ] octahedral–tetrahedral chain in ferrinatrite; (b) the arrangement of [ M ( T Ø) 3 ] chains in ferrinatrite; (c) the [ M 2 ( T Ø 4 ) 3 Ø 5 ] chain in the minerals of the copiapite group; (d) the structure of copiapite; (e) the chain in destinezite; (f
Journal Article
Published: 01 October 2006
The Canadian Mineralogist (2006) 44 (5): 1227–1237.
... solutions on the ambient minerals and rocks. Minerals of the copiapite group display a remarkably wide range of compositional variations ( Atencio et al. 1996 ). The general formula of these minerals is A Fe 3+ 4 (SO 4 ) 6 (OH) 2 (H 2 O) 20 , where A = Fe 2+ (copiapite sensu stricto ), Mg 2...
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Journal Article
Published: 01 June 2009
The Canadian Mineralogist (2009) 47 (3): 509–524.
..., pickeringite, alunogen, epsomite, hexahydrite, a smectite-group phase, galena, sphalerite, and trace calcite. Rhomboclase and copiapite were identified by XRD in only one <2 μm sample. The water-soluble sulfates are not pure end-member phases: pickeringite and epsomite contain Zn (Zn:Mg atomic ratio from 1...
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Journal Article
Published: 01 April 2011
The Canadian Mineralogist (2011) 49 (2): 605–614.
... occurrence, other iron sulfates were identified, including alum-(K), “copiapite”, fibroferrite, halotrichite, melanterite, römerite, and voltaite. Volaschioite occurs as radial aggregates of bladed crystals, up to 100 μm in length and less than 5 μm across. The color is yellowish orange with an orange...
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Journal Article
Published: 01 April 2003
Mineralogical Magazine (2003) 67 (2): 263–278.
... of (Fe 0.68 Mg 0.24 Cu 0.05 Zn 0.03 ) ∑1.00 SO 4 .7H 2 O. Melanterite was also found in mixtures with the Fe 2+ salt minerals rozenite and szomolnokite and aluminocopiapite, an Al-rich end-member of the copiapite group. All salt minerals which include melanterite contained a greater mass of Cu to Zn...
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Journal Article
Published: 01 January 2000
Reviews in Mineralogy and Geochemistry (2000) 40 (1): 303–350.
... ·22H 2 O     apjohnite Mn 2+ Al 2 (SO 4 ) 4 ·22H 2 O     wupatkiite Co 2+ Al 2 (SO 4 ) 4 ·22H 2 O     dietrichite ZnAl 2 (SO 4 ) 4 ·22H 2 O     bilinite Fe 2+ Fe 2 3+ (SO 4 ) 4 ·22H 2 O     redingtonite Fe 2+ (Cr,Al) 2 (SO 4 ) 4 ·22H 2 O Copiapite Group (OH-bearing...
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Journal Article
Published: 01 December 2006
The Canadian Mineralogist (2006) 44 (6): 1431–1446.
... to sequester Cu and Zn is well known ( Frau 2000 , Jambor et al. 2000 , Hammarstrom et al. 2005 ). Structural substitutions of several heavy metals have been also documented in epsomite-, hexahydrite- and chalcanthite-group minerals ( Jambor et al. 2000 ). The ability of copiapite-group minerals...
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Journal Article
Published: 01 November 2013
American Mineralogist (2013) 98 (11-12): 1943–1965.
... by the same doublet with δ = 0.41 mm/s and Δ = 1.14–1.21 mm/s. Botryogen is also related to and in the same Strunz classification group as copiapite; recall from discussion above that copiapite also has a doublet with parameters of δ = 0.42–0.43 mm/s and Δ = 0.77–0.80 mm/s. In addition to the doublets with Δ...
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Journal Article
Published: 01 October 2013
Mineralogical Magazine (2013) 77 (7): 2975–2988.
... Nicolas Meisser. The new mineral was found in a sandstone matrix and is associated with chalcanthite, copiapite, ferrinatrite, gypsum, johannite and another new Na-bearing uranyl sulfate, belakovskiite (IMA2013-075). Meisserite is a secondary mineral formed by the post-mining weathering of uraninite...
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Journal Article
Published: 01 February 2012
The Canadian Mineralogist (2012) 50 (1): 65–72.
..., and hexahydrite, but other ammonium minerals (salammoniac, mascagnite, clairite, boussingaultite, efremovite, koktaite, mohrite, ammoniojarosite, godovikovite, letovicite) as well as native sulfur, millosevichite, alunogen, metavoltine, voltaite, gypsum, anhydrite, halotrichite, butlerite, jarosite, and copiapite...
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Journal Article
Published: 01 December 2010
The Canadian Mineralogist (2010) 48 (6): 1465–1468.
... ( Demartin et al. 2010b ). Structural changes related to a variation in composition at the octahedral sites have also been observed for other sulfates of ferric iron, such as those in the copiapite group ( Majzlan & Michallik 2007 ), and can also be expected in other open structures...
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Journal Article
Published: 01 June 2013
Mineralogical Magazine (2013) 77 (4): 453–465.
..., secondary mineral occurring in a sulfate assemblage with anhydrite, botryogen, chalcanthite, copiapite, halotrichite, hexahydrite, hydroniumjarosite, pyrite, römerite, rozenite and szomolnokite. Lavender-coloured crystals up to several mm across form dense intergrowths. More rarely crystals occur as drusy...
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