12-15 September 2022
Europe/Rome timezone

Crystal-chemistry of the secondary minerals of the thallium-rich pyrite ores from the Apuan Alps (Tuscany, Italy)

12 Sep 2022, 17:10
10m
-/-/- - Teatrino Basaglia (Parco San Giovanni)

-/-/- - Teatrino Basaglia

Parco San Giovanni

200
Premio Mazzi Session

Speaker

Daniela Mauro (Università degli Studi di Pisa)

Description

The mineralogy of secondary assemblages deriving from the alteration of pyrite ore deposits from the southern sector of the Apuan Alps (Tuscany, Italy) has been investigated. Twenty-five mineral species have been identified so far; among them, eight, showing interesting crystal-chemical features, were fully characterized using X-ray diffraction, chemical analyses, and spectroscopic techniques [1]. The structural description of some previously known minerals (epsomite, wilcoxite, coquimbite, khademite, alum-(K), and voltaite) allowed to improve our knowledge about H-bond systems in sulfates and to assess their role in hosting potentially toxic elements. Moreover, this study permitted the identification of two new mineral species, giacovazzoite, $K_5Fe^{3+}_3O(SO_4)_6(H_2O)_9·H_2O$, from the Monte Arsiccio mine, and bohuslavite, $Fe^{3+}_4(PO_4)_3(SO_4)(OH)(H_2O)_{10}·nH_2O$ (5 < n < 24), from the Buca della Vena mine [2, 3].
Giacovazzoite (Figure 1) is the natural counterpart of the β-Maus’ Salt. It is monoclinic, space group P21/c, with a = 9.48, b = 18.44, c = 18.05 Å, β = 92.6°, V = 3153.6 Å$^3$. Its crystal structure is characterized by a heteropolyhedral $[Fe^{3+}_3O(SO_4)_6(H_2O)_3]^{5-}$ cluster and by an interstitial complex with composition $[K_5(H_2O)_7]^{5+}$. The heteropolyhedral cluster is known in other minerals (metavoltine, scordariite, carlsonite) as well as in some synthetic compounds.
Bohuslavite (Figure 1) is triclinic pseudo-hexagonal, space group P-1, with unit-cell parameters a = 13.38, b = 13.34, c = 10.86 Å, α = 92.8, β = 91.0, γ = 119.9°, V = 1675.7 Å$^3$. This mineral can be considered a new kind of microporous compound, with heteropolyhedral layers with composition $[Fe^{3+}_4(PO_4)_3O(OH)(H_2O)_{10}]$, decorated on both sides by $SO_4$ groups. Additional $H_2O$ groups are hosted in channels running along c as well as in the interlayers.
This work stressed the complexity of sulfates, improving the knowledge of their systematics.

[1] C. Biagioni, D. Mauro, M. Pasero Minerals. 2020, 10, 1092.
[2] C. Biagioni, L. Bindi, D. Mauro, M. Pasero Phys Chem Miner. 2020, 47, 7.
[3] D. Mauro, C. Biagioni, E. Bonaccorsi, U. Hålenius, M. Pasero, H. Skogby, F. Zaccarini, J. Sejkora, J. Plášil, A.R. Kampf, J. Filip, P. Novotný, R. Škoda, T. Witzke Eur J Mineral, 2019, 31, 1033.

Primary author

Daniela Mauro (Università degli Studi di Pisa)

Presentation Materials