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crichtonite

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Journal Article
Published: 10 February 2023
Mineralogical Magazine (2023) 87 (3): 433–442.
...Dmitriy I. Rezvukhin; Sergey V. Rashchenko; Igor S. Sharygin; Vladimir G. Malkovets; Taisia A. Alifirova; Leonid. A. Pautov; Elena N. Nigmatulina; Yurii V. Seryotkin Abstract Two new mineral species of the crichtonite group: botuobinskite, ideally SrFe 2+ (Ti 4+ 12 Cr 3+ 6 )Mg 2 [O 36 (OH) 2...
FIGURES
First thumbnail for: Botuobinskite and mirnyite, two new minerals of th...
Second thumbnail for: Botuobinskite and mirnyite, two new minerals of th...
Third thumbnail for: Botuobinskite and mirnyite, two new minerals of th...
Journal Article
Published: 01 May 2019
American Mineralogist (2019) 104 (5): 761–774.
...Dmitriy I. Rezvukhin; Taisia A. Alifirova; Andrey V. Korsakov; Alexander V. Golovin Abstract Large-ion lithophile elements (LILE)-enriched chromium titanates of the magnetoplumbite (AM 12 O 19 ) and crichtonite (ABC 18 T 2 O 38 ) groups have been recognized as abundant inclusions in orthopyroxene...
FIGURES
First thumbnail for: A new occurrence of yimengite-hawthorneite and <sp...
Second thumbnail for: A new occurrence of yimengite-hawthorneite and <sp...
Third thumbnail for: A new occurrence of yimengite-hawthorneite and <sp...
Journal Article
Published: 01 May 2017
European Journal of Mineralogy (2017) 29 (2): 331–338.
...Xiangkun Ge; Guang Fan; Guowu Li; Ganfu Shen; Zhangru Chen; Yujie Ai Mianningite (IMA 2014-072), ideally (☐,Pb,Ce,Na)(U 4+ ,Mn,U 6+ )Fe 3+ 2 (Ti,Fe 3+ ) 18 O 38 , is a new member of the crichtonite group from the Maoniuping REE deposit, Mianning county, Sichuan province, China. It was found...
Journal Article
Published: 01 April 2015
Mineralogical Magazine (2015) 79 (2): 269–283.
... with I > 3σ( I ). Almeidaite is a member of the crichtonite group with Pb dominant in the A site (with 12-fold coordination) and Zn dominant in the T site (with 4-fold coordination). It is a Zn analogue of senaite and a Pb analogue of landauite. The mineral is named after Professor Fernando Flávio...
FIGURES
First thumbnail for: Almeidaite, Pb(Mn,Y)Zn 2 (Ti,Fe 3+ ) 18 O 36 (O,OH...
Second thumbnail for: Almeidaite, Pb(Mn,Y)Zn 2 (Ti,Fe 3+ ) 18 O 36 (O,OH...
Third thumbnail for: Almeidaite, Pb(Mn,Y)Zn 2 (Ti,Fe 3+ ) 18 O 36 (O,OH...
Journal Article
Published: 01 June 2014
European Journal of Mineralogy (2014) 26 (3): 427–437.
.... The crystal structures of mapiquiroite from these two occurrences were refined to R 1 = 0.028 and 0.032, respectively. Mapiquiroite is isostructural with other members of the crichtonite group. The name mapiquiroite honours four Italian mineral collectors, Riccardo Mazzanti, Luigi Pierotti, Ugo Quilici...
FIGURES
First thumbnail for: Mapiquiroite, (Sr,Pb)(U,Y)Fe 2 (Ti,Fe 3+ ) 18 O 38...
Second thumbnail for: Mapiquiroite, (Sr,Pb)(U,Y)Fe 2 (Ti,Fe 3+ ) 18 O 38...
Third thumbnail for: Mapiquiroite, (Sr,Pb)(U,Y)Fe 2 (Ti,Fe 3+ ) 18 O 38...
Journal Article
Published: 01 October 2012
European Journal of Mineralogy (2012) 24 (6): 1061–1067.
.... The crystal structure was refined to R = 0.0234 for 632 reflections with I o > 2σ( I o ) and is isostructural with senaite and all other members of the crichtonite group. The eight strongest X-ray powder-diffraction lines [ d in Å ( I/I 0 ) ( hkl )] are: 3.417 (100) (024), 3.012 (21) (300), 2.896 (61...
FIGURES
First thumbnail for: Paseroite, PbMn 2+ (Mn 2+ ,Fe 2+ ) 2 (V 5+ ,Ti,Fe ...
Second thumbnail for: Paseroite, PbMn 2+ (Mn 2+ ,Fe 2+ ) 2 (V 5+ ,Ti,Fe ...
Third thumbnail for: Paseroite, PbMn 2+ (Mn 2+ ,Fe 2+ ) 2 (V 5+ ,Ti,Fe ...
Journal Article
Published: 01 July 2006
European Journal of Mineralogy (2006) 18 (4): 493–502.
..., related to crichtonite, landauite and davidite-(Ce,La), may represent potentially new members of the crichtonite group. They display compositional zoning, and are associated with diverse oxide minerals, albite and alkali feldspar. Our compositions (EMP) suggest that the “large cations” (Sr, Na, K...
FIGURES
First thumbnail for: Sr-Na-REE titanates of the <span class="search-hig...
Second thumbnail for: Sr-Na-REE titanates of the <span class="search-hig...
Third thumbnail for: Sr-Na-REE titanates of the <span class="search-hig...
Journal Article
Published: 01 November 2005
European Journal of Mineralogy (2005) 17 (6): 933–942.
...Pierre-Alain WÜLSER; Nicolas MEISSER; Joël BRUGGER; Kurt SCHENK; Stefan ANSERMET; Michel BONIN; François BUSSY Abstract Cleusonite, (Pb,Sr)(U 4+ ,U 6+ ) (Fe 2+ ,Zn) 2 (Ti,Fe 2+ ,Fe 3+ ) 18 (O,OH) 38 , is a new member of the crichtonite group. It was found at two occurrences in greenschist facies...
FIGURES
First thumbnail for: Cleusonite, (Pb,Sr) (U 4+ , U 6+ ) (Fe 2+ , Zn) 2 ...
Second thumbnail for: Cleusonite, (Pb,Sr) (U 4+ , U 6+ ) (Fe 2+ , Zn) 2 ...
Third thumbnail for: Cleusonite, (Pb,Sr) (U 4+ , U 6+ ) (Fe 2+ , Zn) 2 ...
Journal Article
Published: 01 January 2004
European Journal of Mineralogy (2004) 16 (1): 171–175.
...Paolo ORLANDI; Marco PASERO; Nicola ROTIROTI; Filippo OLMI; Francesco DEMARTIN; Yves MOËLO Abstract Gramaccioliite-(Y) is a new mineral within the crichtonite group. It was found in the gneiss of the Hercynian Massif of Argentera, at Sambuco (Stura Valley, Piedmont, Italy). It occurs as black...
FIGURES
First thumbnail for: Gramaccioliite-(Y), a new mineral of the <span cla...
Journal Article
Published: 01 August 1997
American Mineralogist (1997) 82 (7-8): 807–811.
...Paolo Orlandi; Marco Pasero; Giuseppe Duchi; Filippo Olmi Abstract Dessauite, a new mineral in the crichtonite group, occurs within cavities in calcite veins as tabular {001} rhombohedral, black, millimeter-sized crystals at Buca della Vena Mine, Apuan Alps (Tuscany, Italy). It is associated...
Journal Article
Published: 01 April 1985
American Mineralogist (1985) 70 (3-4): 414–418.
...A. P. Jones; V. Ekambaram Abstract Titanate minerals of the crichtonite series (AM 21 O 38 , A = Sr in crichtonite; M = Ti, Fe, Cr) reported from mantle peridotite xenoliths associated with kimberlites appear to be solid solutions of several named end members (mostly Ba, Sr, K, Ca) that contain...
Journal Article
Published: 01 June 1983
American Mineralogist (1983) 68 (5-6): 494–505.
... of the AM 21 O 38 series, characterized by predominant A-specific, large cations (Sr = crichtonite; Na = landauite; Pb = senaite; Ca = loveringite, and U + REE = davidite), and by M-formula small cations which are dominantly Ti, Cr, Fe, Mg, Zr, and Nb. Approximately 70% of the A-site is filled by either Ba...
Journal Article
Published: 01 February 1978
American Mineralogist (1978) 63 (1-2): 28–36.
... of 0.043. Loveringite is isostructural with senaite and crichtonite, with a structure based on a nine-layer ( hhc ···) close-packed anion lattice in which the A cation occupies an anion site and the M cations are ordered into 19 octahedral and 2 tetrahedral sites per unit cell. Microprobe analyses...
Journal Article
Published: 01 December 1976
American Mineralogist (1976) 61 (11-12): 1203–1212.
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Published: 10 February 2023
Table 12. Crichtonite-group minerals approved by IMA–CNMNC and their structural formula. Data are from the IMA List of Minerals, updated in November 2022 (Pasero, 2022 ). *Φ = 38 for all members of the crichtonite group. Possible additional cations in octahedral sites (Armbruster and Kunz
Image
Transmitted-light images showing mineral relationships and occurrences of crichtonite-group minerals in silicates. CGM = crichtonite-group mineral; Spl = spinel; Rt = rutile; Opx = orthopyroxene; Grt = garnet. (Color online.)
Published: 01 May 2019
Figure 4. Transmitted-light images showing mineral relationships and occurrences of crichtonite-group minerals in silicates. CGM = crichtonite-group mineral; Spl = spinel; Rt = rutile; Opx = orthopyroxene; Grt = garnet. (Color online.)
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(a) Ba–K–Ca+Sr+Na+LREE ternary diagram and (b) Al2O3–Na/(Na+K) binary plot showing compositions of inclusions of crichtonite-group minerals in Chompolo pyropes. ‘LIMA’ stands for lindsleyite–mathiasite series minerals in metasomatised peridotite xenoliths, mostly from South African kimberlites. Compositional fields for the ‘LIMA’ series and ‘Inclusions in pyrope’ are after (Rezvukhin et al., 2018 and references therein). The ‘Chompolo trend’ shows enrichment of the crichtonite-group minerals from Chompolo pyropes in Ba – a feature that is not typical to crichtonite-group minerals as inclusions in pyropes from other localities.
Published: 12 January 2022
Fig. 6. (a) Ba–K–Ca+Sr+Na+LREE ternary diagram and (b) Al 2 O 3 –Na/(Na+K) binary plot showing compositions of inclusions of crichtonite-group minerals in Chompolo pyropes. ‘LIMA’ stands for lindsleyite–mathiasite series minerals in metasomatised peridotite xenoliths, mostly from South African
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A-site occupancy of the studied yimengite-hawthorneite (a) and crichtonite-group minerals (b) showed within Ba–K–Ca+Sr+Na+LREE ternary space in comparison with literature data. 1 = inclusions of yimengite-hawthorneite in orthopyroxene (this study); 2 = mantle-derived magnetoplumbite-group minerals reported in metasomatized xenoliths and as inclusions in diamonds worldwide (Dong et al. 1984; Haggerty et al. 1989; Nixon and Condliffe 1989; Zhao 1991; Lu and Chou 1994; Zhou et al. 1996; Sobolev et al. 1997; Bulanova et al. 2004; Lu et al. 2007); 3 = haggertyite from the Prairie Creek lamproite, U.S.A. (Grey et al. 1998; Velde 2000); 4 = inclusions of crichtonite-group minerals in orthopyroxene (this study); 5 = crichtonite-group minerals in interstitial oxide intergrowths (this study); 6 = inclusions of crichtonite-group minerals in pyrope (this study). Compositional fields for “Inclusions in pyrope” (red) and “LIMA (South Africa)” (green) are after (Rezvukhin et al. 2018) and references therein. (Color online.)
Published: 01 May 2019
Figure 6. A-site occupancy of the studied yimengite-hawthorneite ( a ) and crichtonite-group minerals ( b ) showed within Ba–K–Ca+Sr+Na+LREE ternary space in comparison with literature data. 1 = inclusions of yimengite-hawthorneite in orthopyroxene (this study); 2 = mantle-derived magnetoplumbite
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Chemical variability in members of the crichtonite group with M0 = Sr or Pb and M1 = Y or U. Data are from Bermanec et al. (1992), Orlandi et al. (1997, 2004b) and Wülser et al. (2005).
Published: 01 June 2014
Fig. 4 Chemical variability in members of the crichtonite group with M0 = Sr or Pb and M1 = Y or U. Data are from Bermanec et al . (1992) , Orlandi et al . (1997 , 2004b ) and Wülser et al . (2005) .
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Published: 01 July 2006
Table 2. Structural formulae of the Sr-Na-REE titanate minerals of the crichtonite group from the Khibina complex.