Angelo Paone graduated with a thesis in geology and geochemistry of the volcanic rocks of Pantelleria at Università degli Studi di Napoli “Federico IIâ€. The work concerned also the analyses of major and trace elements of the the rhyolites and trachytes of Pantelleria. He also produced 14C data from the paleosoil and charcoal dating some eruptive events in Pantelleria. Then, He got a grant under the form of a master to visit the USGS in Reston, VA where I was trained in all aspects of isotope geology. He was trained in the rock preparation, chemical analyses and mass spectrometry functioning for the following parent-daughter isotopes Rb-Sr, Sm-Nd, U-Pb. He also acquired knowledge in stable isotope work (Oxygen and Boron). The mass spectrometries Finnigan Mat 251, 262 have been mastered during such time. Successively, He got a PhD from the University of Naples which He used to continue to visit the USGS in Reston. During such time, He produced a full database for the volcanic rocks of Campania region (Somma-Vesuvius, Campi Flegrei, Roccamonfina, Ventotene, Ponza Island). He has fully introduced in the major elements analysed by wavelength-dispersive XRF; H2O+ and H2O- wet chemical analysis; Rb, Sr, Ba, Zr, and Y determined by energy-dispersive XRF; Cl, F, and Ni determined by photometry; Be, B, Cr, Li, Mo, Pb, Sn, Nb, W measured using ICP-MS and AAS. REE and Hf, Ta, Th, Zn, Co, Sb, U, and Cs analysed by INAA. Above this, I continued my work on Sr-Nd-Pb isotope. During this time, He also acquired knowledge on the analyses of U-Th disequilibrium in fact some analyses were obtained from volcanic rocks of Somma-Vesuvius. During my PhD, He was also fully trained in fluid and melt inclusion petrology. After that, He obtained a Marie Curie Fellowship at University of Bristol and mainly He worked on the interpretation modeling such data and also producing some data on water, CO2 and solubility data. After the Marie Curie, He went for a post doc in Volcanology and petrology at University of Naples where He worked in solving some problems linked between the evolved composition of the magma erupted (Campanian Ignimbrites, Campanian Volcanic Subprovince) and their volume, trying to find a model that would have explained the presence of such abundance of material erupted in such area. Also He worked with Italian carbonatites in relation to the Roman Comagmatic Province trying to found a combined origin suggesting an implication on the genesis of carbonatites woldwide. He also used an exchange grant with Norwey and in particular with the University of Bergen. The grant was used to produce new U-Th data for dating a speleothem from Southern Italy in order to built a robust oxygen and carbon isotopes profile to investigate the microclimatic condition in the Holocene of Campania region. In this moment, He looking for position where research can be applied to volcanic system-ore deposits modeling, and not only, and with much emphasis to numerical modeling and isotope laboratory work . In addition, however, the strong commitment will be to produce paper in the first rank journal. The last and not the least, and I strongly emphasis this aspect, He will be committed to work in the university even for 18 hours a day to have success on the projects and to let the projects to became of international value.
Other Editorial Board Members
Iliana Veneva Lazova-Borisova
Institute of Cryobiology and Food Technologies
View ProfileDanielle Resende de Aguiar
Commission of Monitoring and Evaluation - Municipal
View ProfileMohamad Alsaleh Wang Mo
Institute of Tropical Agriculture & Food Security
View ProfileSyeda Hijab Zehra
Lithuanian Research Centre for Agriculture and Forestry
View ProfileIsidro Requejo Luis Maconetzín
National Institute of Agricultural and Livestock Forestry Research
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