Zobrazeno 1 - 10
of 93
pro vyhledávání: '"P. Gamaletsos"'
Publikováno v:
Materials Proceedings, Vol 5, Iss 1, p 45 (2021)
To tackle the challenge of bauxite residue (BR), generated during the alumina production, as well as to recover some of its metal content, three combinatory H2-based processes were utilized. Firstly, Greek BR was mixed with NaOH to produce water solu
Externí odkaz:
https://doaj.org/article/b4c5501db16f4fd7932ed30dcd3d5131
Akademický článek
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Autor:
Evangelos Tzamos, Platon N. Gamaletsos, Giovanni Grieco, Micol Bussolesi, Anthimos Xenidis, Anastasios Zouboulis, Dimitrios Dimitriadis, Yiannis Pontikes, Athanasios Godelitsas
Publikováno v:
Minerals, Vol 10, Iss 3, p 236 (2020)
Antimony is a common metalloid occurring in the form of Sb-sulfides and sulfosalts, in various base and noble metal deposits. It is also present in corresponding metallurgical products (concentrates) and, although antimony has been considered a penal
Externí odkaz:
https://doaj.org/article/aeea008174fa41c28ad26809c8516368
Akademický článek
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Metastable iron sulfides are involved in a series of biotic and abiotic processes in the marine environment, including the mineralization of organic matter. However, naturally occurring metastable iron (mono)sulfide minerals are rarely reported in ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::a01965011d021b158e3ed61ad10a6228
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3220508
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3220508
Autor:
Joerg Goettlicher, P. Gamaletsos, Kalotina Geraki, Ralph Steininger, A. Borst, Adrian A. Finch, Henrik Friis, Nicola J. Horsburgh
Publikováno v:
Mineralogical magazine, 84 (1), 19–34
Borst, A M, Finch, A A, Friis, H, Horsburgh, N J, Gamaletsos, P N, Goettlicher, J, Steininger, R & Geraki, K 2020, ' Structural state of rare earth elements in eudialyte-group minerals ', Mineralogical Magazine, vol. 84, no. 1, pp. 19-34 . https://doi.org/10.1180/mgm.2019.50
Borst, A M, Finch, A A, Friis, H, Horsburgh, N J, Gamaletsos, P N, Goettlicher, J, Steininger, R & Geraki, K 2020, ' Structural state of rare earth elements in eudialyte-group minerals ', Mineralogical Magazine, vol. 84, no. 1, pp. 19-34 . https://doi.org/10.1180/mgm.2019.50
Eudialyte-group minerals (EGM) attract global interest as potential resources for high-field-strength elements (e.g. Zr, Nb, Ta, and rare-earth elements), i.e. critical materials for modern technologies. They are particularly valued for their relativ
Autor:
Michail Samouhos, Chrysanthi Nomikou, P. Gamaletsos, Petros Tsakiridis, Athanasios Apostolikas, Maria Taxiarchou, Athanasios Godelitsas, Janez Zavašnik
Publikováno v:
Geochemistry. 79:268-279
Nickeliferous laterite ores from two typical central Greece deposits (Larymna and Evia), currently used in the LARCO GMMSA smelting plant to produce ferronickel, were characterized using a combination of diffraction, microscopic, and analytical techn
Autor:
Maria Economou-Eliopoulos, Ralph Steininger, Jörg Göttlicher, P. Gamaletsos, Sofia Kalatha, Athanasios Godelitsas
Publikováno v:
Journal of Geochemical Exploration. 194:189-197
Bauxitic Fe-Ni-laterite ore from the Patitira mine in Lokris area (Greece) contains assemblages of unusual As-bearing goethite-type phases in samples with significant organic matter. The material was initially characterized by bulk ICP-MS and SEM-EDS
Publikováno v:
Journal of Sustainable Metallurgy. 5:20-47
More recent data of Greek bauxites from the Parnassos-Ghiona active mines prove that rare earth elements (REEs) occur mainly in the form of authigenic/diagenetic LREE3+ carbonate and phosphate minerals (bastnasite/parisite group and florencite). Bulk
Autor:
M.M. Abad-Ortega, P. Gamaletsos, Ralph Steininger, Athanasios Godelitsas, Michael G. Stamatakis, Maria Perraki, Jörg Göttlicher, Ioannis Mitsis
Publikováno v:
Applied Clay Science. 162:362-374
Chromium-bearing clays occurring at Crommyonia (Soussaki), Greece, are studied in detail. In this area Mesozoic ultramafic ophiolitic rocks were affected by a Pliocene volcanic activity continuing, nowadays, with intense post-volcanic phenomena. Part