Mckelveyite group minerals – Part 4: Alicewilsonite-(YLa), Na2Sr2YLa (CO3)6  ⋅  3H2O, a new lanthanum-dominant species from the Paratoo mine, Australia

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Abstract 2 Sr2 YLa (CO3) 6  ⋅ 2 O, was found together with kamphaugite-(Y), paratooite-(Y), bastnäsite-(La), and decrespignyite-(Y) coating along fractures in dolomite at the Paratoo copper mine, South Australia, Australia. It occurs as pale pink to colourless pseudohexagonal tabular crystals up to 150 µ m in size. The streak is white; the lustre is vitreous. The mineral has no cleavage. D calc - 3 - α = β =  1.582 (2), γ =  1.592 (2), 2V (meas.) = = 2 O 7.43, CaO 2.00, SrO 18.43, BaO 1.64, Y2 O3 9.59, La2 O3 11.74, Pr2 O3 1.29, Nd2 O3 5.74, Sm2 O3 0.44, Eu2 O3 0.09, Gd2 O3 0.95, Dy2 O3 1.15, Ho2 O3 0.25, Er2 O3 0.89, Yb2 O3 0.29, CO2 29.78, H2 O 6.18, total 97.88. The empirical formula calculated on the basis of six cations with 3 H2 O molecules is as follows: Na2.10 Ca0.31 Sr1.56 Ba0.10 Y0.74 La0.63 Pr0.07 Nd0.30 Sm0.03 Eu0.01 Gd0.04 Dy0.05 Ho0.01 Er0.04 Yb0.01 (CO3) 5.92 (H2 O) 3. The mineral is triclinic, P a =  8.9839 (2), b =  8.9728 (3), c =  6.7441 (2) Å, α =  102.812 (2)°, β =  116.424 (2)°, γ =  60.128 (2)°, and V =  422.17 (2) Å3 and Z =  1. The strongest reflections of the powder X-ray diffraction pattern [d I 1 ‾ 0, 2 ‾ 1 ‾ 1 ‾ 11, 210, 1 ‾ 2 ‾ 2 ‾ 1 ‾ 1 ‾ 1, 121), 2.819 (96)(002, 1 ‾ 12, 211, 1 ‾ 2 ‾ 3 ‾ 01, 030, 3 ‾ 3 ‾ 2 ‾ 21, 4 ‾ 2 ‾ 2 ‾ 4 ‾ 2 ‾ 22, 003, 420, 2 ‾ 4 ‾ 3 ‾ 03, 301, 03 ‾ 2, 032, 3 ‾ 3 ‾ R 1 =  0.058).

Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Mckelveyite group minerals – Part 4: Alicewilsonite-(YLa), Na₂Sr₂YLa (CO₃)₆ ⋅ 3H₂O, a new lanthanum-dominant species from the Paratoo mine, Australia ; volume:36 ; number:2 ; year:2024 ; pages:301-310 ; extent:10
European journal of mineralogy ; 36, Heft 2 (2024), 301-310 (gesamt 10)

Creator: Lykova, Inna
Rowe, Ralph
Poirier, Glenn
Friis, Henrik
Helwig, Kate

DOI: 10.5194/ejm-36-301-2024

URN: urn:nbn:de:101:1-2024032803284746637453

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 14.08.2025, 10:49 AM CEST

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Lykova, Inna
Rowe, Ralph
Poirier, Glenn
Friis, Henrik
Helwig, Kate

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Mckelveyite group minerals – Part 4: Alicewilsonite-(YLa), Na<sub>2</sub>Sr<sub>2</sub>YLa (CO<sub>3</sub>)<sub>6</sub>&thinsp; ⋅ &thinsp;3H<sub>2</sub>O, a new lanthanum-dominant species from the Paratoo mine, Australia

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Other Objects (12)

Mckelveyite group minerals – Part 2: Alicewilsonite-(YCe), Na<sub>2</sub>Sr<sub>2</sub>YCe (CO<sub>3</sub>)<sub>6</sub>&thinsp; ⋅ &thinsp;3H<sub>2</sub>O, a new species

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Mckelveyite group minerals – Part 4: Alicewilsonite-(YLa), Na<sub>2</sub>Sr<sub>2</sub>YLa (CO<sub>3</sub>)<sub>6</sub> ⋅ 3H<sub>2</sub>O, a new lanthanum-dominant species from the Paratoo mine, Australia

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Redefinition of beraunite, Fe<sup>3+</sup><sub>6</sub>(PO<sub>4</sub>)<sub>4</sub>O (OH)<sub>4</sub> ⋅ 6H<sub>2</sub>O, and discreditation of the name eleonorite: a re-investigation of type material from the Hrbek Mine (Czech Republic)

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Spatiotemporal variations of the <italic>δ</italic>(O<sub>2</sub> ∕ N<sub>2</sub>), CO<sub>2</sub> and <italic>δ</italic>(APO) in the troposphere over the western North Pacific

Redefinition of beraunite, Fe<sup>3+</sup><sub>6</sub>(PO<sub>4</sub>)<sub>4</sub>O (OH)<sub>4</sub> ⋅ 6H<sub>2</sub>O, and discreditation of the name eleonorite: a re-investigation of type material from the Hrbek Mine (Czech Republic)

A modeling approach to investigate drivers, variability and uncertainties in O<sub>2</sub> fluxes and O<sub>2</sub> : CO<sub>2</sub> exchange ratios in a temperate forest

Mckelveyite group minerals – Part 2: Alicewilsonite-(YCe), Na<sub>2</sub>Sr<sub>2</sub>YCe (CO<sub>3</sub>)<sub>6</sub> ⋅ 3H<sub>2</sub>O, a new species

Mckelveyite group minerals – Part 3: Bainbridgeite-(YCe), Na<sub>2</sub>Ba<sub>2</sub>YCe (CO<sub>3</sub>)<sub>6</sub> ⋅ 3H<sub>2</sub>O, a new species from Mont Saint-Hilaire, Canada

Regerite, KFe<sub>6</sub>(PO<sub>4</sub>)<sub>4</sub>(OH)<sub>7</sub>(H<sub>2</sub>O)<sub>6</sub> ⋅ 4H<sub>2</sub>O, the first new mineral species from the Kreuzberg pegmatite, Pleystein, Oberpfalz, Bavaria, Germany

Hochleitnerite, (K (H<sub>2</sub>O)) Mn<sub>2</sub>(Ti<sub>2</sub>Fe)(PO<sub>4</sub>)<sub>4</sub>O<sub>2</sub>(H<sub>2</sub>O)<sub>10</sub> ⋅ 4H<sub>2</sub>O, a new paulkerrite-group mineral, from the Hagendorf-Süd pegmatite, Oberpfalz, Bavaria, Germany

Dacostaite, K (Mg<sub>2</sub>Al)(Mg (H<sub>2</sub>O)<sub>6</sub>)<sub>2</sub>(AsO<sub>4</sub>)<sub>2</sub>F<sub>6</sub> ⋅ 2H<sub>2</sub>O, a new fluoride–arsenate mineral from the Cetine di Cotorniano Mine (Tuscany, Italy)

Bonacinaite, Sc (AsO<sub>4</sub>) ⋅ 2H<sub>2</sub>O, the first scandium arsenate

Spatiotemporal variations of the <italic>δ</italic>(O<sub>2</sub> ∕ N<sub>2</sub>), CO<sub>2</sub> and <italic>δ</italic>(APO) in the troposphere over the western North Pacific

Redefinition of beraunite, Fe<sup>3+</sup><sub>6</sub>(PO<sub>4</sub>)<sub>4</sub>O (OH)<sub>4</sub> ⋅ 6H<sub>2</sub>O, and discreditation of the name eleonorite: a re-investigation of type material from the Hrbek Mine (Czech Republic)

A modeling approach to investigate drivers, variability and uncertainties in O<sub>2</sub> fluxes and O<sub>2</sub> : CO<sub>2</sub> exchange ratios in a temperate forest