A set of 23 vesbine-bearing samples from Vesuvius volcano (Italy), preserved in the collection of the Royal Mineralogical Museum of Naples, University Federico II (RMMN), have been investigated to identify the mineral assemblages and investigate their mode of formation. In the late nineteenth century, fumarole-related yellow patinas coating some historical lavas from Vesuvius were believed by Scacchi to contain a new element, vesbium, similar to vanadium in a mineral he called vesbine. Subsequent studies rejected vesbium and showed that vesbine was a poorly-defined mixture of copper vanadates and halides. The vesbine samples studied here, consist of yellowish to yellow-green-blue encrustations on Vesuvius lavas and have been analysed by combined optical microscopy, SEM-EDS, XRPD, FTIR and TEM-HRTEM-EDX analyses. Results reveal complex mineral associations, including vanadates, halides, carbonates, oxides, silicates, tungstates/molybdates and sulfates. The vanadates correspond to mottramite, volborthite and vanadinite; subordinate amounts of descloizite were detected by XRPD and FTIR investigations. Several different elements have been detected in the vanadates, including Mn, Zn and As. The occurrence of wulfenite- and stolzite-rich phases indicates the presence of Mo and W, along with Pb, in the mineralizing fluids. Mn-rich phases, commonly in mixtures with silicates and vanadates, were also observed. These minerals are formed by a combination of different processes, including rock-fluids interactions, gas-water interactions, and alteration/oxidation of primary fumarolic minerals. Temperatures for the depositions of the vanadates-bearing assemblages are suggested as being in the range 100 and 400 °C.
Pellino, A., Balassone, G., Abad, I., Altomare, A., Bellatreccia, F., Cappelletti, P., et al. (2024). Re-examination of vesbine in vanadate-rich sublimate-related associations of Vesuvius (Italy): mineralogical features and origin. THE AMERICAN MINERALOGIST [10.2138/am-2023-9126].
Re-examination of vesbine in vanadate-rich sublimate-related associations of Vesuvius (Italy): mineralogical features and origin
Bellatreccia F.;
2024-01-01
Abstract
A set of 23 vesbine-bearing samples from Vesuvius volcano (Italy), preserved in the collection of the Royal Mineralogical Museum of Naples, University Federico II (RMMN), have been investigated to identify the mineral assemblages and investigate their mode of formation. In the late nineteenth century, fumarole-related yellow patinas coating some historical lavas from Vesuvius were believed by Scacchi to contain a new element, vesbium, similar to vanadium in a mineral he called vesbine. Subsequent studies rejected vesbium and showed that vesbine was a poorly-defined mixture of copper vanadates and halides. The vesbine samples studied here, consist of yellowish to yellow-green-blue encrustations on Vesuvius lavas and have been analysed by combined optical microscopy, SEM-EDS, XRPD, FTIR and TEM-HRTEM-EDX analyses. Results reveal complex mineral associations, including vanadates, halides, carbonates, oxides, silicates, tungstates/molybdates and sulfates. The vanadates correspond to mottramite, volborthite and vanadinite; subordinate amounts of descloizite were detected by XRPD and FTIR investigations. Several different elements have been detected in the vanadates, including Mn, Zn and As. The occurrence of wulfenite- and stolzite-rich phases indicates the presence of Mo and W, along with Pb, in the mineralizing fluids. Mn-rich phases, commonly in mixtures with silicates and vanadates, were also observed. These minerals are formed by a combination of different processes, including rock-fluids interactions, gas-water interactions, and alteration/oxidation of primary fumarolic minerals. Temperatures for the depositions of the vanadates-bearing assemblages are suggested as being in the range 100 and 400 °C.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
