Affiliation:
1. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA
2. Dipartimento di Scienze della Terra, dell’Ambiente e della Vita (DISTAV), Università di Genova, Corso Europa 26, 16132 Genova, Italy
Abstract
Cortesognoite (IMA 2014-029), CaV2Si2O7(OH)2·H2O, is a new vanadium silicate mineral that occurs within V-bearing lawsonite in association with vanadiocarpholite, chalcocite, quartz, minor poppiite, roscoelite, vanadomalayaite and volborthite in a silicified wood hosted in Mn-ore-bearing metacherts from the Molinello manganese mine in the Graveglia Valley, Northern Apennines, Liguria, Italy. The mean chemical composition of type cortesognoite by electron probe microanalysis is (wt%) SiO2 34.33, V2O3 31.38, CaO 15.80, Al2O3 7.69, MnO 0.14, FeO 0.09, MgO 0.06, TiO2 0.02 and H2O 10.29, totaling 99.80, giving rise to an empirical formula of (Ca0.99Mn0.01)(V1.47Al0.53Mg0.01)Si2.00O7(OH)2·H2O. The end-member formula is CaV2Si2O7(OH)2·H2O. Cortesognoite has the Cmcm lawsonite structure with a = 5.85(1) Å, b = 8.79(1) Å, c = 13.13(1) Å, V = 675(1) Å3 and Z = 4 as revealed by electron back-scatter diffraction. The calculated density using the measured composition is 3.44 g/cm3. Cortesognoite is a secondary alteration phase, formed with V-bearing lawsonite by multi-stage hydrothermal processes that occurred in the silicified fossil wood. The mineral name is in honor of Luciano Cortesogno, professor of petrography at University of Genova, Italy.
Funder
Ministero dell’Istruzione, dell’Università e delle Ricerca
Subject
Inorganic Chemistry,Condensed Matter Physics,General Materials Science,General Chemical Engineering
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