Articles | Volume 37, issue 4
https://doi.org/10.5194/ejm-37-437-2025
https://doi.org/10.5194/ejm-37-437-2025
Research article
 | 
10 Jul 2025
Research article |  | 10 Jul 2025

Fibrous tourmaline from San Piero in Campo (Elba, Italy)

Giovanni B. Andreozzi, Dario Di Giuseppe, Alessandro F. Gualtieri, Valentina Scognamiglio, Laura Fornasini, Danilo Bersani, Tommaso Giovanardi, Federico Lugli, and Federico Pezzotta

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Cited articles

Aggarwal, S. K. and You, C. F.: A review on the determination of isotope ratios of boron with mass spectrometry, Mass Spectr. Rev., 36, 499–519, 2017. 
Altieri, A., Pezzotta, F., Skogby, H., Hålenius, U., and Bosi, F.: Dark-coloured Mn-rich overgrowths in an elbaitic tourmaline crystal from the Rosina pegmatite, San Piero in Campo, Elba Island, Italy: witness of late-stage opening of the geochemical system, Mineral. Mag., 87, 130–142, 2023a. 
Altieri, A., Pezzotta, F., Andreozzi, G. B., Skogby, H., and Bosi, F.: Genetic model for the color anomalies at the termination of pegmatitic gem tourmaline crystals from the island of Elba, Italy, Eur. J. Mineral., 35, 755–771, https://doi.org/10.5194/ejm-35-755-2023, 2023b. 
Andreozzi, G. B., Bosi, F., Celata, B., Capizzi, L. S., Stagno, V., and Beckett-Brown, C. E.: Crystal-chemical behavior of Fe2+ in tourmaline dictated by structural stability: insights from a schorl with formula NaY(Fe22+Al)Z(Al5Fe2+)(Si6O18)(BO3)3(OH)3(OH,F) from Seagull batholith (Yukon Territory, Canada), Phys. Chem. Min., 47, 1–9, 2020. 
Andreozzi, G. B., Gori, C., Skogby, H., Hålenius, U., Altieri, A., and Bosi, F.: Insights from the compositional evolution of a multi-coloured, zoned tourmaline from the Cruzeiro pegmatite, Minas Gerais, Brazil, Eur. J. Mineral., 37, 1–12, 2025. 
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Short summary
An unusual tourmaline was studied using a multi-analytical approach. The sample comes from a granitic pegmatite on the island of Elba and consists of three generations of tourmaline: green prismatic tourmaline, a dark fibrous cap, and colourless acicular single crystals. The most likely scenario for its formation involves the miarolitic cavity fracturing due to mechanical shock, the subsequent circulation of the highly reactive cavity fluids, and the leaching of accessory biotite in the surrounding pegmatite.
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