Minasgeraisite-(Y)

Minasgeraisite-(Y) is a discredited mineral species that was originally described as a rare member of the gadolinite supergroup with the chemical formula Y₂CaBe₂Si₂O₁₀. Typically appearing as minute, purplish-lavender rosettes in late-stage cavities of zoned granitic pegmatites, it was first identified at the José Pinto quarry in 1986 in Jaguaraçu, Minas Gerais, Brazil. The mineral was named after its type locality and approved by the International Mineralogical Association (IMA) under the name ''minasgeraisite-(Y)''. Subsequent crystallographic and chemical analyses of the type material, as well as of comparable specimens from Norway and Central Europe, led to the mineral's discreditation in 2023 under IMA–CNMNC Proposal 23-F. It is now regarded as a bismuth- and manganese-rich variety of hingganite-(Y).

Origins

Minasgeraisite-(Y) was described as a new member of the gadolinite group in a paper by Eugene E. Foord et al. published in 1986, with its type locality designated as the Jaguaraçu granitic pegmatite in Minas Gerais, Brazil. The mineral was discovered at the Mr. José Pinto quarry, a site known for its complex, zoned pegmatitic formations. Its name, approved by the International Mineralogical Association (IMA) under proposal 83-90, was later modified to minasgeraisite-(Y) to conform to IMA nomenclature standards for rare-earth element minerals. The initial discovery of minasgeraisite-(Y) stemmed from investigations led by Foord following the collection of fine milarite crystals at the site in 1980. During this work, small amounts of an unidentified lilac-colored mineral were found in the drusy cavities. In 2021, minasgeraisite-(Y) was assigned the IMA symbol ''Mgr-Y''.

Subsequent re-investigations of material from the type locality, including crystallographic and chemical studies, have led to the discreditation of minasgeraisite-(Y) as a distinct species in 2023. The discreditation was made based on IMA-CNMNC Proposal 23-F. Modern analyses have demonstrated that the material originally described as minasgeraisite-(Y) is structurally and compositionally consistent with bismuth-, manganese-rich varieties of hingganite-(Y).

Occurrence

Minasgeraisite-(Y) occurs as a late-stage accessory mineral. Other minerals associated with minasgeraisite-(Y) include milarite, albite, quartz, muscovite, hematite, amazonite, orthoclase, almandine–spessartine, magnetite, churchite-(Y), elbaite, pyrite, cerussite, pyromorphite, and anatase. It was originally described from the Jaguaraçu granitic pegmatite in Minas Gerais, Brazil, specifically at the José Pinto quarry in the municipality of Jaguaraçu, which is recognized as its type locality. It occurs as a rare, accessory mineral that formed during the late stages of pegmatite crystallization. Within the zoned, complex pegmatite, it appears in small druses and is typically associated with minerals such as milarite, albite, quartz, and muscovite. The mineral is found as minute sheaf-like crystals less than 3–5 µm across, forming rosettes that range from 0.2 to 1.0 mm in diameter, which may occur singly or in aggregates.

Although minasgeraisite-(Y) was initially described only from its Brazilian type locality, subsequent studies identified chemically similar material at the Heftetjern pegmatite in southern Norway, which was interpreted as a second occurrence. Additional reports have noted similar compositions from the Krenn quarry in Germany, the Vlastějovice region in the Czech Republic, and Rigó Hill in Hungary. However, these specimens did not match the ideal end-member composition, and the researcher Oleg S. Vereshchagin considered the Brazilian locality to be the only confirmed source of minasgeraisite-(Y) as originally described.

Structure

Minasgeraisite-(Y) was originally described as a member of the gadolinite supergroup, a group of minerals characterized by the general formula A₂MQ₂T₂O₈φ₂, where A, M, Q, T represent distinct crystallographic sites occupied by different cations, and φ denotes anions such as hydroxyl or oxygen. The crystal structure is typically understood as composed of alternating layers parallel to the (100) plane within a monoclinic symmetry, most commonly space group ''P2''₁/c. One layer consists of interconnected TO₄ and QO₄ tetrahedra forming sheets with a characteristic 4.8² net, featuring four- and eight-membered rings where silicon alternates with beryllium or boron. The A and M cations reside in polyhedral sites situated between these tetrahedral sheets.

In the initial description, minasgeraisite-(Y) was assigned a monoclinic symmetry with space group ''P2''₁/a and an end-member formula Y₂CaBe₂Si₂O₁₀. This formulation suggested calcium as the dominant cation in the sixfold-coordinated M site, which was unusual given calcium's typical preference for larger coordination sites in other gadolinite-group minerals.

Subsequent single-crystal studies, however, revealed that material from the type locality and comparable samples from Norway exhibited triclinic symmetry with space group P1, deviating from the monoclinic norm seen in related minerals such as datolite and hingganite-(Y). This reduction in symmetry is attributed to significant cation ordering at the A sites. In this triclinic structure, the single A site splits into four distinct and non-equivalent sites (denoted W1 through W4), occupied by bismuth, calcium, and rare earth elements (primarily yttrium and other heavy lanthanides). Bismuth predominates at W1, calcium at W2, and yttrium and other REEs occupy W3 and W4, demonstrating nearly complete cation ordering.

Characteristics

Hand specimens of minasgeraisite-(Y) tend to be in a purplish-lavender color. Minasgeraisite-(Y) is transparent in hand sample with a sub-vitreous, resinous, dull luster and a pale bluish-green streak. The mineral is brittle and breaks along its fiber contacts. Its observed specific gravity is 4.29, with a hardness of 6–7 on the Mohs scale.

When viewed with polarized light under a petrographic microscope, minasgeraisite-(Y) appears colorless, pale grayish yellow, and lavender purple and moderately exhibits pleochroism. It is biaxial positive and has a high optic angle (or 2V). When measured along different crystallographic directions, its refractive indices are nα = 1.740, nβ = 1.754, and nγ = 1.786. This gives it a birefringence of 0.046.

References

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Minerals described in 1986
Triclinic minerals
Yttrium minerals
Calcium minerals
Beryllium minerals