Zobrazeno 1 - 10
of 124
pro vyhledávání: '"Ni-laterite"'
Autor:
Alexandra Anifadi, Olga Sykioti, Konstantinos Koutroumbas, Emmanuel Vassilakis, Charalampos Vasilatos, Emil Georgiou
Publikováno v:
Remote Sensing, Vol 16, Iss 13, p 2295 (2024)
Currently, the global shift towards green energy is at the forefront of efforts introducing a new era, thus rendering exploration for critical raw materials essential. To this purpose, the utilization of advanced machine learning methods in remote se
Externí odkaz:
https://doaj.org/article/c449ff20a99249acb750996caa5cdf0d
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The Morowali Ni-laterite deposit is located in the East Sulawesi Ophiolite, which is a large ophiolite belt on Sulawesi Island, Indonesia. The Morowali deposit is developed on a laterite profile due to ophiolite weathering, with saprolite, limonite,
Externí odkaz:
https://doaj.org/article/d630ab9ce8c64f89b27b001c63a58f76
Autor:
Matheus Lamas Machado, Claudio Gerheim Porto, Licia Santoro, Francesco Putzolu, Reiner Neumann, Artur Bastos Neto, Helena Polivanov, Richard Herrington
Publikováno v:
Brazilian Journal of Geology, Vol 51, Iss 3 (2021)
Abstract The Santa Fé Ni laterite deposit (Brazil) developed as a consequence of weathering of serpentinized dunites that produced a regolith in which the main Ni ore zone is a ferruginous saprolite with chlorite as the main ore-carrier along with N
Externí odkaz:
https://doaj.org/article/73030272dd304d8a9be41ba2e8f148f6
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
Cristina Villanova-de-Benavent, Jordi Cama, Josep M. Soler, Cristina Domènech, Salvador Galí, Joaquín A. Proenza
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Digital.CSIC. Repositorio Institucional del CSIC
instname
Universidad de Barcelona
Digital.CSIC. Repositorio Institucional del CSIC
instname
In this study we tested the dissolution kinetics of three garnierite types (serpentine-, talc- and sepiolite-dominated) at pH of 3 and 5 and room temperature by means of flow-through experiments. The samples selected for the study cover a wide range
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10c7a1dc836f2dd474458862539c7ac2
https://api.elsevier.com/content/abstract/scopus_id/85132322602
https://api.elsevier.com/content/abstract/scopus_id/85132322602
Autor:
Yoram Teitler, Sylvain Favier, Jean-Paul Ambrosi, Brice Sevin, Fabrice Golfier, Michel Cathelineau
Publikováno v:
Minerals; Volume 12; Issue 5; Pages: 615
Minerals
Minerals, 2022, 12 (5), pp.615. ⟨10.3390/min12050615⟩
Minerals
Minerals, 2022, 12 (5), pp.615. ⟨10.3390/min12050615⟩
Scandium (Sc) is used in several modern industrial applications. Recently, significant Sc concentrations (~100 ppm) were reported in some nickel-cobalt lateritic ores, where Sc may be valuably co-produced. However, Sc is typically not included in rou
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The Morowali Ni-laterite deposit is located in the East Sulawesi Ophiolite, which is a large ophiolite belt on Sulawesi Island, Indonesia. The Morowali deposit is developed on a laterite profile due to ophiolite weathering, with saprolite, limonite,
Autor:
Thomas Aiglsperger, González-Jiménez, José M., Proenza, Joaquín A., Salvador Galí, FRANCISCO GERALDO LONGO, Griffin, William L., O’reilly, Suzanne Y.
Publikováno v:
Minerals, Vol 11, Iss 1083, p 1083 (2021)
BASE-Bielefeld Academic Search Engine
BASE-Bielefeld Academic Search Engine
In this short communication, we present preliminary data on the Re-Os isotopic systematics of platinum-group minerals (PGM) recovered from different horizons in the Falcondo Ni-laterite in the Dominican Republic. The results show differences in the O