Spherical aggregates of microcrystals filling hydrothermal cavities or earthy masses with pale lavender color of probable phosphosiderite were found by one of the authors (F.V.) in the dumps of the Malpensata pegmatite mine. This hydrated Fe phosphate had been identified by means of electron microprobe in wavelength dispersive mode (WDS) and powder Xray diffraction analysis (XRPD). Chemical analyses (Table 1) revealed the following empirical formula (Fe1,02Mn0,02)?1,04(PO4)?2,08H2O, and the XRPD analysis gave the following unitcell parameters a = 5,301(4) Å, b =analysis gave the following unitcell parameters a = 5,301(4) Å, b = 9,778(6) Å, c = 8,726(4) Å e ? = 90,3(1) ° in close agreement with those reported for this mineral species.

La fosfosiderite della Malpensata: prima segnalazione a Piona, Lecco

2014

Abstract

Spherical aggregates of microcrystals filling hydrothermal cavities or earthy masses with pale lavender color of probable phosphosiderite were found by one of the authors (F.V.) in the dumps of the Malpensata pegmatite mine. This hydrated Fe phosphate had been identified by means of electron microprobe in wavelength dispersive mode (WDS) and powder Xray diffraction analysis (XRPD). Chemical analyses (Table 1) revealed the following empirical formula (Fe1,02Mn0,02)?1,04(PO4)?2,08H2O, and the XRPD analysis gave the following unitcell parameters a = 5,301(4) Å, b =analysis gave the following unitcell parameters a = 5,301(4) Å, b = 9,778(6) Å, c = 8,726(4) Å e ? = 90,3(1) ° in close agreement with those reported for this mineral species.
2014
Istituto per la Dinamica dei Processi Ambientali - IDPA - Sede Venezia
Istituto di Geologia Ambientale e Geoingegneria - IGAG
Italiano
38
3
178
181
4
Sì, ma tipo non specificato
phosphosiderite
Piona albite pegmatite
phosphate
Malpensata dike
1
info:eu-repo/semantics/article
262
Pietro Vignola Paolo Gentile Andrea Risplendente Franco Vanini,
01 Contributo su Rivista::01.01 Articolo in rivista
none
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/229953
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