Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada

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Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada. / Anzolini, Chiara; Siva-Jothy, William K.; Locock, Andrew J.; Nestola, Fabrizio; Balić-Zunić, Tonči; Alvaro, Matteo; Chinn, Ingrid L.; Stachel, Thomas; Graham Pearson, D.

I: American Mineralogist, Bind 107, Nr. 8, 2022, s. 1635-1642.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Anzolini, C, Siva-Jothy, WK, Locock, AJ, Nestola, F, Balić-Zunić, T, Alvaro, M, Chinn, IL, Stachel, T & Graham Pearson, D 2022, 'Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada', American Mineralogist, bind 107, nr. 8, s. 1635-1642. https://doi.org/10.2138/am-2022-8098

APA

Anzolini, C., Siva-Jothy, W. K., Locock, A. J., Nestola, F., Balić-Zunić, T., Alvaro, M., Chinn, I. L., Stachel, T., & Graham Pearson, D. (2022). Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada. American Mineralogist, 107(8), 1635-1642. https://doi.org/10.2138/am-2022-8098

Vancouver

Anzolini C, Siva-Jothy WK, Locock AJ, Nestola F, Balić-Zunić T, Alvaro M o.a. Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada. American Mineralogist. 2022;107(8):1635-1642. https://doi.org/10.2138/am-2022-8098

Author

Anzolini, Chiara ; Siva-Jothy, William K. ; Locock, Andrew J. ; Nestola, Fabrizio ; Balić-Zunić, Tonči ; Alvaro, Matteo ; Chinn, Ingrid L. ; Stachel, Thomas ; Graham Pearson, D. / Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada. I: American Mineralogist. 2022 ; Bind 107, Nr. 8. s. 1635-1642.

Bibtex

@article{13ff0039baeb4c2ba77ac4cfa689057c,
title = "Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Ku{\'e}, Canada",
abstract = "Heamanite-(Ce) (IMA 2020-001), ideally (K0.5Ce0.5)TiO3, is a new perovskite-group mineral found as an inclusion in a diamond from the Gahcho Ku{\'e} mine in the Northwest Territories, Canada. It occurs as brown, translucent single crystals with an average maximum dimension of ~80 μm, associated with rutile and calcite. The luster is adamantine, and the fracture conchoidal. Heamanite-(Ce) is the K-analog of loparite-(Ce), ideally (NaCe)Ti2O6. The Mohs hardness is estimated to be 5½ by comparison to loparite-(Ce), and the calculated density is 4.73(1) g/cm3. Electron microprobe wavelength-dispersive spectrometric analysis (average of 34 points) yielded: CaO 10.70, K2O 7.38, Na2O 0.16, Ce2O3 13.77, La2O3 8.22, Pr2O3 0.84, Nd2O3 1.59, SrO 6.69, BaO 2.96, ThO2 0.36, PbO 0.15, TiO2 45.77, Cr2O3 0.32, Al2O3 0.10, Fe2O3 0.09, Nb2O5 0.87, UO3 0.01, total 99.98 wt%. The empirical formula, based on 3 O atoms, is: [(K0.268Na0.009)ς0.277(Ce0.143La0.086Pr0.009Nd0.016)ς0.254(Ca0.326Sr0.110Ba0.033Pb0.001)ς0.470Th0.002]ς1.003 (Ti0.979Nb0.011Cr0.007Al0.003Fe0.002)ς1.002O3. The Goldschmidt tolerance factor for this formula is 1.003. Heamanite-(Ce) is cubic, space group Pm3m, with unit-cell parameter a = 3.9129(9) {\AA}, and volume V = 59.91(4) {\AA}3 (Z = 1). The crystal structure was solved using single-crystal X-ray diffraction data and refined to R1(F) = 2.61%. Heamanite-(Ce) has the aristotypic perovskite structure and adopts the same structure as isolueshite and tausonite. The six strongest diffraction lines are [dobs in angstroms (I in percentages) (hkl)]: 2.764 (100) (110), 1.954 (41) (200), 1.596 (36) (211), 1.045 (16) (321), 1.236 (13) (310), and 1.382 (10) (220). The Raman spectrum of heamanite-(Ce) shows two broad bands at 560 and 787 cm-1, with no bands observed above 1000 cm-1. Heamanite-(Ce) is named after Larry Heaman, a renowned scientist in the field of radiometric dating applied to diamond-bearing kimberlites, mantle-derived eclogites, and lamprophyre dikes. The dominant REE should appear as a Levinson suffix, hence heamanite-(Ce). ",
keywords = "crystal structure, diamond inclusion, Gahcho Ku{\'e}, Heamanite-(Ce), loparite-(Ce), mantle, new mineral, perovskite",
author = "Chiara Anzolini and Siva-Jothy, {William K.} and Locock, {Andrew J.} and Fabrizio Nestola and Ton{\v c}i Bali{\'c}-Zuni{\'c} and Matteo Alvaro and Chinn, {Ingrid L.} and Thomas Stachel and {Graham Pearson}, D.",
note = "Publisher Copyright: {\textcopyright} 2022 Mineralogical Society of America.",
year = "2022",
doi = "10.2138/am-2022-8098",
language = "English",
volume = "107",
pages = "1635--1642",
journal = "American Mineralogist",
issn = "0003-004X",
publisher = "Mineralogical Society of America",
number = "8",

}

RIS

TY - JOUR

T1 - Heamanite-(Ce), (K0.5Ce0.5)TiO3, a new perovskite supergroup mineral found in diamond from Gahcho Kué, Canada

AU - Anzolini, Chiara

AU - Siva-Jothy, William K.

AU - Locock, Andrew J.

AU - Nestola, Fabrizio

AU - Balić-Zunić, Tonči

AU - Alvaro, Matteo

AU - Chinn, Ingrid L.

AU - Stachel, Thomas

AU - Graham Pearson, D.

N1 - Publisher Copyright: © 2022 Mineralogical Society of America.

PY - 2022

Y1 - 2022

N2 - Heamanite-(Ce) (IMA 2020-001), ideally (K0.5Ce0.5)TiO3, is a new perovskite-group mineral found as an inclusion in a diamond from the Gahcho Kué mine in the Northwest Territories, Canada. It occurs as brown, translucent single crystals with an average maximum dimension of ~80 μm, associated with rutile and calcite. The luster is adamantine, and the fracture conchoidal. Heamanite-(Ce) is the K-analog of loparite-(Ce), ideally (NaCe)Ti2O6. The Mohs hardness is estimated to be 5½ by comparison to loparite-(Ce), and the calculated density is 4.73(1) g/cm3. Electron microprobe wavelength-dispersive spectrometric analysis (average of 34 points) yielded: CaO 10.70, K2O 7.38, Na2O 0.16, Ce2O3 13.77, La2O3 8.22, Pr2O3 0.84, Nd2O3 1.59, SrO 6.69, BaO 2.96, ThO2 0.36, PbO 0.15, TiO2 45.77, Cr2O3 0.32, Al2O3 0.10, Fe2O3 0.09, Nb2O5 0.87, UO3 0.01, total 99.98 wt%. The empirical formula, based on 3 O atoms, is: [(K0.268Na0.009)ς0.277(Ce0.143La0.086Pr0.009Nd0.016)ς0.254(Ca0.326Sr0.110Ba0.033Pb0.001)ς0.470Th0.002]ς1.003 (Ti0.979Nb0.011Cr0.007Al0.003Fe0.002)ς1.002O3. The Goldschmidt tolerance factor for this formula is 1.003. Heamanite-(Ce) is cubic, space group Pm3m, with unit-cell parameter a = 3.9129(9) Å, and volume V = 59.91(4) Å3 (Z = 1). The crystal structure was solved using single-crystal X-ray diffraction data and refined to R1(F) = 2.61%. Heamanite-(Ce) has the aristotypic perovskite structure and adopts the same structure as isolueshite and tausonite. The six strongest diffraction lines are [dobs in angstroms (I in percentages) (hkl)]: 2.764 (100) (110), 1.954 (41) (200), 1.596 (36) (211), 1.045 (16) (321), 1.236 (13) (310), and 1.382 (10) (220). The Raman spectrum of heamanite-(Ce) shows two broad bands at 560 and 787 cm-1, with no bands observed above 1000 cm-1. Heamanite-(Ce) is named after Larry Heaman, a renowned scientist in the field of radiometric dating applied to diamond-bearing kimberlites, mantle-derived eclogites, and lamprophyre dikes. The dominant REE should appear as a Levinson suffix, hence heamanite-(Ce).

AB - Heamanite-(Ce) (IMA 2020-001), ideally (K0.5Ce0.5)TiO3, is a new perovskite-group mineral found as an inclusion in a diamond from the Gahcho Kué mine in the Northwest Territories, Canada. It occurs as brown, translucent single crystals with an average maximum dimension of ~80 μm, associated with rutile and calcite. The luster is adamantine, and the fracture conchoidal. Heamanite-(Ce) is the K-analog of loparite-(Ce), ideally (NaCe)Ti2O6. The Mohs hardness is estimated to be 5½ by comparison to loparite-(Ce), and the calculated density is 4.73(1) g/cm3. Electron microprobe wavelength-dispersive spectrometric analysis (average of 34 points) yielded: CaO 10.70, K2O 7.38, Na2O 0.16, Ce2O3 13.77, La2O3 8.22, Pr2O3 0.84, Nd2O3 1.59, SrO 6.69, BaO 2.96, ThO2 0.36, PbO 0.15, TiO2 45.77, Cr2O3 0.32, Al2O3 0.10, Fe2O3 0.09, Nb2O5 0.87, UO3 0.01, total 99.98 wt%. The empirical formula, based on 3 O atoms, is: [(K0.268Na0.009)ς0.277(Ce0.143La0.086Pr0.009Nd0.016)ς0.254(Ca0.326Sr0.110Ba0.033Pb0.001)ς0.470Th0.002]ς1.003 (Ti0.979Nb0.011Cr0.007Al0.003Fe0.002)ς1.002O3. The Goldschmidt tolerance factor for this formula is 1.003. Heamanite-(Ce) is cubic, space group Pm3m, with unit-cell parameter a = 3.9129(9) Å, and volume V = 59.91(4) Å3 (Z = 1). The crystal structure was solved using single-crystal X-ray diffraction data and refined to R1(F) = 2.61%. Heamanite-(Ce) has the aristotypic perovskite structure and adopts the same structure as isolueshite and tausonite. The six strongest diffraction lines are [dobs in angstroms (I in percentages) (hkl)]: 2.764 (100) (110), 1.954 (41) (200), 1.596 (36) (211), 1.045 (16) (321), 1.236 (13) (310), and 1.382 (10) (220). The Raman spectrum of heamanite-(Ce) shows two broad bands at 560 and 787 cm-1, with no bands observed above 1000 cm-1. Heamanite-(Ce) is named after Larry Heaman, a renowned scientist in the field of radiometric dating applied to diamond-bearing kimberlites, mantle-derived eclogites, and lamprophyre dikes. The dominant REE should appear as a Levinson suffix, hence heamanite-(Ce).

KW - crystal structure

KW - diamond inclusion

KW - Gahcho Kué

KW - Heamanite-(Ce)

KW - loparite-(Ce)

KW - mantle

KW - new mineral

KW - perovskite

U2 - 10.2138/am-2022-8098

DO - 10.2138/am-2022-8098

M3 - Journal article

AN - SCOPUS:85135523162

VL - 107

SP - 1635

EP - 1642

JO - American Mineralogist

JF - American Mineralogist

SN - 0003-004X

IS - 8

ER -

ID: 316817635