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laueite

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Journal Article
Published: 01 December 2016
Mineralogical Magazine (2016) 80 (7): 1243–1254.
...I. E. Grey; E. Keck; W. G. Mumme; A. Pring; C. M. Macrae; A. M. Glenn; C. J. Davidson; F. L. Shanks; S. J. Mills Abstract Kummerite, ideally Mn 2+ Fe 3+ Al(PO 4 ) 2 (OH) 2 ·8H 2 O, is a new secondary phosphate mineral belonging to the laueite group, from the Hagendorf-Süd pegmatite, Hagendorf...
FIGURES | View All (6)
Journal Article
Published: 01 April 2015
Mineralogical Magazine (2015) 79 (2): 243–246.
...S. J. Mills; I. E. Grey Abstract A new nomenclature scheme has been set up for the laueite supergroup of minerals, which have the general formula M 1 2+ M 2 3+ M 3 3+ ( X O 4 ) 2 (OH) 2 ·8H 2 O, where M 1 = Fe 2+ , Mg 2+ or Mn 2+ ; M 2/ M 3 = Al 3+ or Fe 3+ ; and X O 4 = PO 4 or AsO 4 . The laueite...
FIGURES
Journal Article
Published: 01 April 2015
Mineralogical Magazine (2015) 79 (2): 309–319.
...I. E. Grey; E. Keck; W. G. Mumme; C. M. MacRae; J. R. Price; A. M. Glenn; C. J. Davidson Abstract Crystals of laueite, Mn 2+ Fe 2 3 + (PO 4 ) 2 (OH) 2 ·8H 2 O, from the Cornelia mine open cut, Hagendorf Süd, Bavaria, are zoned due to aluminium incorporation at the iron sites, with analysed Al 2 O 3...
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Journal Article
Published: 01 April 2014
American Mineralogist (2014) 99 (4): 607–611.
...Ricardo Scholz; Nikita V. Chukanov; Luiz A.D. Menezes Filho; Daniel Atencio; Leonardo Lagoeiro; Fernanda M. Belotti; Mário L.S.C. Chaves; Antônio W. Romano; Paulo R. Brandão; Dmitriy I. Belakovskiy; Igor Pekov Abstract Césarferreiraite, Fe 2+ Fe 2 3+ (AsO 4 ) 2 (OH) 2 ·8H 2 O, is a new laueite...
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Journal Article
Published: 01 August 2012
European Journal of Mineralogy (2012) 24 (4): 717–726.
... octahedral-tetrahedral layer is that of the laueite type and belongs to the laueite isomer of the laueite-stewartite-pseudolaueite-metavauxite group of structural and geometrical isomers. Maghrebite is an arsenate analogue of gordonite and is the first natural member of the laueite group to contain arsenate...
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Journal Article
Published: 01 October 1969
American Mineralogist (1969) 54 (9-10): 1312–1323.
... are topologically distinct. The details of the distortions of the coordination octahedra can be accounted for by the extended electrostatic valence rule, provided one considers the contributions of the hydrogen atoms. It is proposed that pseudolaueite and laueite are not true polymorphs because laueite contains...
Journal Article
Published: 01 December 1965
American Mineralogist (1965) 50 (11-12): 1884–1892.
...Paul Brian Moore Abstract Laueite, Mn 2+ Fe 2 3+ (OH) 2 (PO 4 ) 2 (H 2 O)6·2H 2 O, triclinic P 1 , a = 5.28, b = 10.66, c = 7,14 Å, α = 107°55’, β =110 o 59’, γ = 7l°07’, Z = 1, has two known isotypes and three polymorphs. Its crystal structure consists of infinite chains of vertex-linked oxygen...
Image
The crystal structures of laueite and curetonite: (a) laueite projected onto (010); (b) laueite projected onto (001); (H2O) groups not bonded to any cations are not shown; (c) curetonite projected onto (010); (d) curetonite projected onto (001). (Feϕ6) and (Alϕ6) octahedra are dot-shaded and 44-net-shaded, respectively; Mn2+ and Ba are shown as shaded circles, selected (H2O) groups are shown as grey circles.
Published: 01 January 2002
Figure 26. The crystal structures of laueite and curetonite: (a) laueite projected onto (010); (b) laueite projected onto (001); (H 2 O) groups not bonded to any cations are not shown; (c) curetonite projected onto (010); (d) curetonite projected onto (001). (Feϕ 6 ) and (Alϕ 6 ) octahedra
Image
[0 0 1] projections of the structures of (a) laueite and (b) earlshannonite, showing perfect matching of the dimensions within the (0 0 1) planes for the two structures, which is the basis for epitactic growth of earlshannonite on laueite shown in Fig. 10 (Online version in colour).
Published: 01 September 2018
Fig. 9 [0 0 1] projections of the structures of (a) laueite and (b) earlshannonite, showing perfect matching of the dimensions within the (0 0 1) planes for the two structures, which is the basis for epitactic growth of earlshannonite on laueite shown in Fig. 10 (Online version in colour).
Journal Article
Published: 01 September 2018
European Journal of Mineralogy (2018) 30 (5): 1007–1020.
...Fig. 9 [0 0 1] projections of the structures of (a) laueite and (b) earlshannonite, showing perfect matching of the dimensions within the (0 0 1) planes for the two structures, which is the basis for epitactic growth of earlshannonite on laueite shown in Fig. 10 (Online version in colour). ...
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Image
Published: 01 June 2002
TABLE 6. MINERALS OF THE LAUEITE AND RELATED GROUPS
Journal Article
Published: 01 June 1994
American Mineralogist (1994) 79 (5-6): 545–549.
... that constitutes the structural unit of the mineral. The sheets are linked by tenfold-coordinated interstitial Ba atoms. The M(TO 4 ) ϕ 2 sheet is topologically identical to the structural unit in laueite (Moore, 1965, 1975), but the intersheet linkage by Ba atoms is very different from that in laueite, which...
Image
The heteropolyhedral (010) sheet in laueite. Small grey and blue spheres are hydrogen and oxygen.
Published: 01 December 2016
Fig. 1. The heteropolyhedral (010) sheet in laueite. Small grey and blue spheres are hydrogen and oxygen.
Image
SEM BSE image of Zn-bearing earlshannonite rods epitactic on (Zn + Mg)-bearing laueite.
Published: 01 September 2018
Fig. 10 SEM BSE image of Zn-bearing earlshannonite rods epitactic on (Zn + Mg)-bearing laueite.
Image
Backscattered electron image showing zoning due to Al/Fe variations in Al-bearing laueite.
Published: 01 April 2015
F ig . 2. Backscattered electron image showing zoning due to Al/Fe variations in Al-bearing laueite.
Image
The heteropolyhedral (0 1 0) sheet in laueite. Butlerite-type (B) and kröhnkite-type (K) chains are indicated by arrows.
Published: 01 April 2015
F ig . 3. The heteropolyhedral (0 1 0) sheet in laueite. Butlerite-type (B) and kröhnkite-type (K) chains are indicated by arrows.
Image
Laueite heteropolyhedral sheet. Small grey, light blue and dark blue spheres are coordinated oxygen, hydroxyl and water, respectively.
Published: 01 April 2015
F ig . 1. Laueite heteropolyhedral sheet. Small grey, light blue and dark blue spheres are coordinated oxygen, hydroxyl and water, respectively.
Image
Backscattered electron image showing Al-bearing laueite (L) and associated minerals, beraunite (B), frondelite (F) and jahnsite (J).
Published: 01 April 2015
F ig . 1. Backscattered electron image showing Al-bearing laueite (L) and associated minerals, beraunite (B), frondelite (F) and jahnsite (J).
Image
Connectivity between laueite sheets. Small grey, light blue and dark blue spheres are coordinated oxygen, hydroxyl and water, respectively. Large blue spheres are interlayer water molecules.
Published: 01 April 2015
F ig . 2. Connectivity between laueite sheets. Small grey, light blue and dark blue spheres are coordinated oxygen, hydroxyl and water, respectively. Large blue spheres are interlayer water molecules.
Image
Scatter plots for (a) Mg apfuvs. Zn apfu and (b) Zn + Mg apfuvs. Mn apfu from EMP analyses of (Zn + Mg)-bearing laueite crystals (Online version in colour).
Published: 01 September 2018
Fig. 8 Scatter plots for (a) Mg apfu vs. Zn apfu and (b) Zn + Mg apfu vs. Mn apfu from EMP analyses of (Zn + Mg)-bearing laueite crystals (Online version in colour).