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    Rights statement: https://www.cambridge.org/core/journals/mineralogical-magazine/article/occurrence-of-wakefieldite-a-rare-earth-element-vanadate-in-the-rhyolitic-joe-lott-tuff-utah-usa/227B7FFBA9E68B85D426B713372D3BC1

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The occurrence of wakefieldite, a rare earth element vanadate, in the rhyolitic Joe Lott Tuff, Utah, USA

Research output: Contribution to Journal/Magazine › Journal article › peer-review

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The occurrence of wakefieldite, a rare earth element vanadate, in the rhyolitic Joe Lott Tuff, Utah, USA. / Bagiński, B.; MacDonald, R.; Belkin, H.E. et al.
In: Mineralogical Magazine, Vol. 84, No. 1, 01.02.2020, p. 109-116.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Bagiński, B, MacDonald, R, Belkin, HE, Kotowski, J, Jokubauskas, P & Marciniak-Maliszewska, B 2020, 'The occurrence of wakefieldite, a rare earth element vanadate, in the rhyolitic Joe Lott Tuff, Utah, USA', Mineralogical Magazine, vol. 84, no. 1, pp. 109-116. https://doi.org/10.1180/mgm.2019.66

APA

Bagiński, B., MacDonald, R., Belkin, H. E., Kotowski, J., Jokubauskas, P., & Marciniak-Maliszewska, B. (2020). The occurrence of wakefieldite, a rare earth element vanadate, in the rhyolitic Joe Lott Tuff, Utah, USA. Mineralogical Magazine, 84(1), 109-116. https://doi.org/10.1180/mgm.2019.66

Vancouver

Bagiński B, MacDonald R, Belkin HE, Kotowski J, Jokubauskas P, Marciniak-Maliszewska B. The occurrence of wakefieldite, a rare earth element vanadate, in the rhyolitic Joe Lott Tuff, Utah, USA. Mineralogical Magazine. 2020 Feb 1;84(1):109-116. Epub 2019 Oct 14. doi: 10.1180/mgm.2019.66

Author

Bagiński, B. ; MacDonald, R. ; Belkin, H.E. et al. / The occurrence of wakefieldite, a rare earth element vanadate, in the rhyolitic Joe Lott Tuff, Utah, USA. In: Mineralogical Magazine. 2020 ; Vol. 84, No. 1. pp. 109-116.

Bibtex

@article{6e2de055bb464da3a94e16685a4b7e42,
title = "The occurrence of wakefieldite, a rare earth element vanadate, in the rhyolitic Joe Lott Tuff, Utah, USA",
abstract = "The high-silica rhyolitic Joe Lott Tuff was erupted at 19.2 ± 0.4 Ma from the Mount Belknap caldera, SW Utah. Certain units in the tuff contain two species of wakefieldite, the Nd- A nd Y-dominant types. They occur in disseminated streaks and patches in association with rhodochrosite, calcite, Fe oxide, cerite-(Ce), and a Mn silicate (caryopilite?), thought to have been deposited from hydrothermal fluids. The wakefieldites contain the highest levels of As (≤15.34 wt.% As2O5) and P (≤5.7 wt.% P2O5) yet recorded in this mineral, indicating significant solid solution towards chernovite-(Y) and xenotime-(Y). Thorium levels are also unusually high (≤14.2 wt.% ThO2). The source of the hydrothermal fluid(s) is unknown but might be related to uranium mineralisation in the region, in that As, V and U are commonly associated in such deposits. {\textcopyright} 2019 Mineralogical Society of Great Britain and Ireland.",
keywords = "As, Joe Lott Tuff, P and Th enrichment, wakefieldite-(Nd), wakefieldite-(Y), Arsenic, Calcite, Iron oxides, Manganese compounds, Rare earths, Silica, Silicates, Thoria, Uranium deposits, High silicas, Hydrothermal fluids, Mineralisation, Utah , USA, Xenotime(y), Arsenic compounds, arsenic, hydrothermal fluid, mineralization, phosphorus, rare earth element, rhyolite, thorium, vanadate group, United States, Utah",
author = "B. Bagi{\'n}ski and R. MacDonald and H.E. Belkin and J. Kotowski and P. Jokubauskas and B. Marciniak-Maliszewska",
year = "2020",
month = feb,
day = "1",
doi = "10.1180/mgm.2019.66",
language = "English",
volume = "84",
pages = "109--116",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
number = "1",

}

RIS

TY - JOUR

T1 - The occurrence of wakefieldite, a rare earth element vanadate, in the rhyolitic Joe Lott Tuff, Utah, USA

AU - Bagiński, B.

AU - MacDonald, R.

AU - Belkin, H.E.

AU - Kotowski, J.

AU - Jokubauskas, P.

AU - Marciniak-Maliszewska, B.

PY - 2020/2/1

Y1 - 2020/2/1

N2 - The high-silica rhyolitic Joe Lott Tuff was erupted at 19.2 ± 0.4 Ma from the Mount Belknap caldera, SW Utah. Certain units in the tuff contain two species of wakefieldite, the Nd- A nd Y-dominant types. They occur in disseminated streaks and patches in association with rhodochrosite, calcite, Fe oxide, cerite-(Ce), and a Mn silicate (caryopilite?), thought to have been deposited from hydrothermal fluids. The wakefieldites contain the highest levels of As (≤15.34 wt.% As2O5) and P (≤5.7 wt.% P2O5) yet recorded in this mineral, indicating significant solid solution towards chernovite-(Y) and xenotime-(Y). Thorium levels are also unusually high (≤14.2 wt.% ThO2). The source of the hydrothermal fluid(s) is unknown but might be related to uranium mineralisation in the region, in that As, V and U are commonly associated in such deposits. © 2019 Mineralogical Society of Great Britain and Ireland.

AB - The high-silica rhyolitic Joe Lott Tuff was erupted at 19.2 ± 0.4 Ma from the Mount Belknap caldera, SW Utah. Certain units in the tuff contain two species of wakefieldite, the Nd- A nd Y-dominant types. They occur in disseminated streaks and patches in association with rhodochrosite, calcite, Fe oxide, cerite-(Ce), and a Mn silicate (caryopilite?), thought to have been deposited from hydrothermal fluids. The wakefieldites contain the highest levels of As (≤15.34 wt.% As2O5) and P (≤5.7 wt.% P2O5) yet recorded in this mineral, indicating significant solid solution towards chernovite-(Y) and xenotime-(Y). Thorium levels are also unusually high (≤14.2 wt.% ThO2). The source of the hydrothermal fluid(s) is unknown but might be related to uranium mineralisation in the region, in that As, V and U are commonly associated in such deposits. © 2019 Mineralogical Society of Great Britain and Ireland.

KW - As

KW - Joe Lott Tuff

KW - P and Th enrichment

KW - wakefieldite-(Nd)

KW - wakefieldite-(Y)

KW - Arsenic

KW - Calcite

KW - Iron oxides

KW - Manganese compounds

KW - Rare earths

KW - Silica

KW - Silicates

KW - Thoria

KW - Uranium deposits

KW - High silicas

KW - Hydrothermal fluids

KW - Mineralisation

KW - Utah , USA

KW - Xenotime(y)

KW - Arsenic compounds

KW - arsenic

KW - hydrothermal fluid

KW - mineralization

KW - phosphorus

KW - rare earth element

KW - rhyolite

KW - thorium

KW - vanadate group

KW - United States

KW - Utah

U2 - 10.1180/mgm.2019.66

DO - 10.1180/mgm.2019.66

M3 - Journal article

VL - 84

SP - 109

EP - 116

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

IS - 1

ER -