Number of the records: 1
Oldsite, K.sub.2./sub.Fe.sup.2+./sup.[(UO.sub.2./sub.)(SO.sub.4./sub.).sub.2./sub.].sub.2./sub.(H.sub.2./sub.O).sub.8./sub., a new uranyl sulfate mineral from Utah, USA: its description and implications for the formation and occurrences of uranyl sulfate minerals
- 1.0569730 - FZÚ 2024 RIV GB eng J - Journal Article
Plášil, Jakub - Kampf, A.R. - Ma, C. - Desor, J.
Oldsite, K2Fe2+[(UO2)(SO4)2]2(H2O)8, a new uranyl sulfate mineral from Utah, USA: its description and implications for the formation and occurrences of uranyl sulfate minerals.
Mineralogical Magazine. Roč. 87, č. 1 (2023), s. 151-159. ISSN 0026-461X. E-ISSN 1471-8022
R&D Projects: GA ČR(CZ) GA20-11949S
Institutional support: RVO:68378271
Keywords : oldsite * new mineral * uranyl sulfate * crystal structure * Raman spectroscopy * North Mesa mines * supergene weathering * Utah * USA
OECD category: Mineralogy
Impact factor: 2.8, year: 2023
Method of publishing: Open access
Oldsite (IMA2021–075), ideally K2Fe2+[(UO2)(SO4)2]2(H2O)8, is a new uranyl sulfate mineral found on specimens from the North Mesa Mine group, Temple Mountain, San Rafael district, Emery County, Utah, USA. It is a secondary mineral occurring with alum-(K), halotrichite, metavoltine, quartz, römerite, stanleyite, sulfur, szomolnokite, and mathesiusite. In this work the mineral's structure and its properties were studied and the results are presented.
Permanent Link: https://hdl.handle.net/11104/0342139
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Number of the records: 1