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Marsaalamite–(Y), Y(MoO4)OH, a new molybdate mineral from the Um Safi area, Marsa Alam District, Central Eastern Desert of Egypt

Authors

Mahdy,  Nasser Mourad
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Ondrejka,  Martin
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Bačík,  Peter
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Biagioni,  Cristian
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Sejkora,  Jiří
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Uher,  Pavel
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Števko,  Martin
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Förster,  H.-J.
4.3 Geoenergy, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Mikuš,  Tomáš
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Citation

Mahdy, N. M., Ondrejka, M., Bačík, P., Biagioni, C., Sejkora, J., Uher, P., Števko, M., Förster, H.-J., Mikuš, T. (2024 online): Marsaalamite–(Y), Y(MoO4)OH, a new molybdate mineral from the Um Safi area, Marsa Alam District, Central Eastern Desert of Egypt. - Mineralogical Magazine, 1-30.
https://doi.org/10.1180/mgm.2024.103


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5032880
Abstract
Marsaalamite-(Y), ideally Y(MoO4)OH, is a new molybdate mineral discovered in the greisenized Um Safi F-rich granite located in the Marsa Alam District, Central Eastern Desert of Egypt. It typically occurs as inclusions in or intergrowths with F-rich zinnwaldite. It forms micaceous aggregates, with sizes varying from 0.1 to 1 mm. Marsaalamite-(Y) is non-magnetic, white in color, and has an earthy lustre and white streak. It is brittle (34 Mohs) and has basal cleavages {001}. The calculated density is 4.90 g.cm–3 based on the empirical formula and unit-cell parameters refined from X-ray powder diffraction data. Marsaalamite-(Y) is associated with arsenopyrite, baryte, bastnäsite-(Ce), cassiterite, chernovite-(Y), columbite-(Fe), fluocerite-(Ce), fluorite, iron oxy-hydroxides, löllingite, molybdenite, monazite-(Ce), pyrite, quartz, rutile, thorite, wolframite, wulfenite, xenotime-(Y), and several unidentified phases. The empirical 2 formula is (Y0.67Er0.10Dy0.08Yb0.08Ho0.02Lu0.02Tm0.02Ca0.01)Σ1.00 (Mo0.95S0.03As0.01P0.01)Σ1.00 O4.00[(OH)0.88F0.11Cl0.01]Σ1.00; the ideal end member formula is Y(MoO4)(OH). The presence of a hydroxyl group has been confirmed by Raman and infrared spectroscopy, and its concentration has been calculated from the stoichiometry. Marsaalamite-(Y) is the natural (OH)-dominant analogue of synthetic Y(MoO4)F. It is monoclinic, space group P21/c, with unit-cell parameters a = 5.1863(7) Å, b = 12.3203(11) Å, c = 6.6953(7) Å, β = 114.173(8)°, V = 390.30(8) Å3, and Z = 4. Extreme fractionation of the parental halogen-rich, A-type granitic magma triggered the greisenization of the granite. The marsaalamite-(Y) occurred simultaneously with or immediately after the crystallization of F-rich zinnwaldite based on the textural relationship. Therefore, the crystallization of marsaalamite-(Y) was most likely controlled by fluid-induced processes rather than magmatic conditions. The new mineral was approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (CNMNC-IMA) (IMA 2024-050) and named after the Marsa Alam District, Al-Bahr Al- Ahmer Governorate, Egypt