Ferroefremovite, (NH.sub.4./sub.).sub.2./sub.Fe.sup.2+./sup..sub.2./sub.(SO.sub.4./sub.).sub.3./sub., a new mineral from Solfatara di Pozzuoli, Campania, Italy

0545218 - FZÚ 2022 RIV CA eng J - Článek v odborném periodiku
Kasatkin, A.V. - Plášil, Jakub - Škoda, R. - Campostrini, I. - Chukanov, N.V. - Agakhanov, A.A. - Karpenko, V.Y. - Belakovskiy, D. I.
Ferroefremovite, (NH₄)₂Fe²⁺₂(SO₄)₃, a new mineral from Solfatara di Pozzuoli, Campania, Italy.
Canadian Mineralogist. Roč. 59, Jan (2021), s. 59-68. ISSN 0008-4476. E-ISSN 1499-1276
Grant CEP: GA ČR GA17-09161S
Institucionální podpora: RVO:68378271
Klíčová slova: ferroefremovite * sulfate * ammonium * new mineral * Solfatara di Pozzuoli * Italy
Obor OECD: Mineralogy
Impakt faktor: 0.817, rok: 2021
Způsob publikování: Omezený přístup
https://doi.org/10.3749/canmin.1900085

The new sulfate mineral ferroefremovite, ideally (NH4)2Fe2+2(SO4)3, was discovered at the „Bocca Grande“ fumarole, Solfatara di Pozzuoli, Flegrean Volcanic Complex, Naples Province, Campania, Italy. Associated minerals are adranosite, adranosite-(Fe), godovikovite, huizingite-(Al), mascagnite, and opal. Ferroefremovite forms cubic crystals up to 0.1 mm across. The new mineral is colorless and has a vitreous luster and white streak. In this work the mineral's structure and its properties were studied and the results are presented.
Trvalý link: http://hdl.handle.net/11104/0321967