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Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni glacier, Switzerland. / Vereshchagin, Oleg S. ; Britvin, Sergey N. ; Perova, Elena N.; Brusnitsyn, Aleksey I. ; Polekhovsky, Yury S. ; Shilovskikh, Vladimir V. ; Bocharov, Vladimir N. ; van der Burgt, Ate; Cuchet, Stéphane; Meisser, Nicolas.

In: American Mineralogist, Vol. 104, No. 10, 25.10.2019, p. 1469–1480.

Research output: Contribution to journal › Article › peer-review

Harvard

Vereshchagin, OS, Britvin, SN, Perova, EN, Brusnitsyn, AI, Polekhovsky, YS, Shilovskikh, VV, Bocharov, VN, van der Burgt, A, Cuchet, S & Meisser, N 2019, 'Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni glacier, Switzerland', American Mineralogist, vol. 104, no. 10, pp. 1469–1480. https://doi.org/10.2138/am-2019-7028

APA

Vereshchagin, O. S., Britvin, S. N., Perova, E. N., Brusnitsyn, A. I., Polekhovsky, Y. S., Shilovskikh, V. V., Bocharov, V. N., van der Burgt, A., Cuchet, S., & Meisser, N. (2019). Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni glacier, Switzerland. American Mineralogist, 104(10), 1469–1480. https://doi.org/10.2138/am-2019-7028

Vancouver

Vereshchagin OS, Britvin SN, Perova EN, Brusnitsyn AI, Polekhovsky YS, Shilovskikh VV et al. Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni glacier, Switzerland. American Mineralogist. 2019 Oct 25;104(10):1469–1480. https://doi.org/10.2138/am-2019-7028

Author

Vereshchagin, Oleg S. ; Britvin, Sergey N. ; Perova, Elena N. ; Brusnitsyn, Aleksey I. ; Polekhovsky, Yury S. ; Shilovskikh, Vladimir V. ; Bocharov, Vladimir N. ; van der Burgt, Ate ; Cuchet, Stéphane ; Meisser, Nicolas. / Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni glacier, Switzerland. In: American Mineralogist. 2019 ; Vol. 104, No. 10. pp. 1469–1480.

BibTeX

@article{0a7fd1d1753242a4a9f37382dc62f55c,
title = "Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni glacier, Switzerland",
abstract = "Gasparite-(La), La(AsO4), is a new mineral (IMA 2018-079) from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan (type locality) and from alpine fissures in metamorphic rocks of the Wanni glacier, Binn Valley, Switzerland (co-type locality). Gasparite-(La) is named for its dominant lanthanide, according to current nomenclature of rare-earth minerals. The occurrences and parageneses in both localities are distinct: minute isometric grains up to 15 μm in size, associated with friedelite, jacobsite, pennantite, manganhumite series minerals (alleghanyite, sonolite), sarkinite, tilasite, and retzian-(La) are typically embedded into calcite-rhodochrosite veinlets (Ushkatyn-III deposit) vs. elongated crystals up to 2 mm in size in classical alpine fissures in two-mica gneiss without indicative associated minerals (Wanni glacier). Their chemical compositions have been studied by EDX and WDX; crystal-chemical formulas of gasparite-(La) from the Ushkatyn-III deposit (holotype specimen) and Wanni glacier (co-type specimen) are (La0.65Ce0.17Nd0.07Ca0.06Mn0.05Pr0.02)1.02[(As0.70V0.28P0.02)1.00O4] and (La0.59Ce0.37Nd0.02 Ca0.02Th0.01)1.01[(As0.81P0.16Si0.02S0.02)1.01O4], respectively. In polished sections, crystals are yellow and translucent with bright submetallic luster. Selected reflectance values R1/R2 (λ, nm) for the holotype specimen in air are: 11.19/9.05 (400), 11.45/9.44 (500), 10.85/8.81 (600), 11.23/9.08 (700). The structural characteristics of gasparite-(La) were studied by means of EBSD (holotype specimen), XRD, and SREF (co-type specimen). Gasparite-(La) has a monoclinic structure with the space group P21/n. Our studies revealed that gasparite-(La) from the Ushkatyn-III deposit and Wanni glacier have different origins. La/Ce and As/P/V ratios in gasparite-(La) may be used as an indicator of formation conditions.",
keywords = "Binn Valley, Gasparite-(La), Kazakhstan, Mn ores, REE, Switzerland, Ushkatyn-III, Wanni glacier, arsenate, monazite-type structure, new mineral",
author = "Vereshchagin, {Oleg S.} and Britvin, {Sergey N.} and Perova, {Elena N.} and Brusnitsyn, {Aleksey I.} and Polekhovsky, {Yury S.} and Shilovskikh, {Vladimir V.} and Bocharov, {Vladimir N.} and {van der Burgt}, Ate and St{\'e}phane Cuchet and Nicolas Meisser",
year = "2019",
month = oct,
day = "25",
doi = "10.2138/am-2019-7028",
language = "English",
volume = "104",
pages = "1469–1480",
journal = "American Mineralogist",
issn = "0003-004X",
publisher = "Mineralogical Society of America",
number = "10",

}

RIS

TY - JOUR

T1 - Gasparite-(La), La(AsO4), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni glacier, Switzerland

AU - Vereshchagin, Oleg S.

AU - Britvin, Sergey N.

AU - Perova, Elena N.

AU - Brusnitsyn, Aleksey I.

AU - Polekhovsky, Yury S.

AU - Shilovskikh, Vladimir V.

AU - Bocharov, Vladimir N.

AU - van der Burgt, Ate

AU - Cuchet, Stéphane

AU - Meisser, Nicolas

PY - 2019/10/25

Y1 - 2019/10/25

N2 - Gasparite-(La), La(AsO4), is a new mineral (IMA 2018-079) from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan (type locality) and from alpine fissures in metamorphic rocks of the Wanni glacier, Binn Valley, Switzerland (co-type locality). Gasparite-(La) is named for its dominant lanthanide, according to current nomenclature of rare-earth minerals. The occurrences and parageneses in both localities are distinct: minute isometric grains up to 15 μm in size, associated with friedelite, jacobsite, pennantite, manganhumite series minerals (alleghanyite, sonolite), sarkinite, tilasite, and retzian-(La) are typically embedded into calcite-rhodochrosite veinlets (Ushkatyn-III deposit) vs. elongated crystals up to 2 mm in size in classical alpine fissures in two-mica gneiss without indicative associated minerals (Wanni glacier). Their chemical compositions have been studied by EDX and WDX; crystal-chemical formulas of gasparite-(La) from the Ushkatyn-III deposit (holotype specimen) and Wanni glacier (co-type specimen) are (La0.65Ce0.17Nd0.07Ca0.06Mn0.05Pr0.02)1.02[(As0.70V0.28P0.02)1.00O4] and (La0.59Ce0.37Nd0.02 Ca0.02Th0.01)1.01[(As0.81P0.16Si0.02S0.02)1.01O4], respectively. In polished sections, crystals are yellow and translucent with bright submetallic luster. Selected reflectance values R1/R2 (λ, nm) for the holotype specimen in air are: 11.19/9.05 (400), 11.45/9.44 (500), 10.85/8.81 (600), 11.23/9.08 (700). The structural characteristics of gasparite-(La) were studied by means of EBSD (holotype specimen), XRD, and SREF (co-type specimen). Gasparite-(La) has a monoclinic structure with the space group P21/n. Our studies revealed that gasparite-(La) from the Ushkatyn-III deposit and Wanni glacier have different origins. La/Ce and As/P/V ratios in gasparite-(La) may be used as an indicator of formation conditions.

AB - Gasparite-(La), La(AsO4), is a new mineral (IMA 2018-079) from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan (type locality) and from alpine fissures in metamorphic rocks of the Wanni glacier, Binn Valley, Switzerland (co-type locality). Gasparite-(La) is named for its dominant lanthanide, according to current nomenclature of rare-earth minerals. The occurrences and parageneses in both localities are distinct: minute isometric grains up to 15 μm in size, associated with friedelite, jacobsite, pennantite, manganhumite series minerals (alleghanyite, sonolite), sarkinite, tilasite, and retzian-(La) are typically embedded into calcite-rhodochrosite veinlets (Ushkatyn-III deposit) vs. elongated crystals up to 2 mm in size in classical alpine fissures in two-mica gneiss without indicative associated minerals (Wanni glacier). Their chemical compositions have been studied by EDX and WDX; crystal-chemical formulas of gasparite-(La) from the Ushkatyn-III deposit (holotype specimen) and Wanni glacier (co-type specimen) are (La0.65Ce0.17Nd0.07Ca0.06Mn0.05Pr0.02)1.02[(As0.70V0.28P0.02)1.00O4] and (La0.59Ce0.37Nd0.02 Ca0.02Th0.01)1.01[(As0.81P0.16Si0.02S0.02)1.01O4], respectively. In polished sections, crystals are yellow and translucent with bright submetallic luster. Selected reflectance values R1/R2 (λ, nm) for the holotype specimen in air are: 11.19/9.05 (400), 11.45/9.44 (500), 10.85/8.81 (600), 11.23/9.08 (700). The structural characteristics of gasparite-(La) were studied by means of EBSD (holotype specimen), XRD, and SREF (co-type specimen). Gasparite-(La) has a monoclinic structure with the space group P21/n. Our studies revealed that gasparite-(La) from the Ushkatyn-III deposit and Wanni glacier have different origins. La/Ce and As/P/V ratios in gasparite-(La) may be used as an indicator of formation conditions.

KW - Binn Valley

KW - Gasparite-(La)

KW - Kazakhstan

KW - Mn ores

KW - REE

KW - Switzerland

KW - Ushkatyn-III

KW - Wanni glacier

KW - arsenate

KW - monazite-type structure

KW - new mineral

UR - http://www.scopus.com/inward/record.url?scp=85073335882&partnerID=8YFLogxK

U2 - 10.2138/am-2019-7028

DO - 10.2138/am-2019-7028

M3 - Article

VL - 104

SP - 1469

EP - 1480

JO - American Mineralogist

JF - American Mineralogist

SN - 0003-004X

IS - 10

ER -

ID: 46374167