Rare earth elements (REEs) are a group of seventeen elements comprising fifteen lanthanides, scandium, and yttrium. They are not necessarily rare, though their occurrences …
C Moudioh, LS Tamehe, S Ganno, MN Tankwa… - Journal of African Earth …, 2020 - Elsevier
The banded iron formations (BIFs) in the Bipindi greenstone belt (GB) are hosted within metavolcano-sedimentary sequence of the Nyong Group at the northwestern edge of the …
The southeastern part of the Democratic Republic of the Congo locally hosts Proterozoic manganese deposits. The deposits of Kisenge-Kamata are the most significant, but …
J Ai, S Siljeström, N Zhong, J Chen, T Wang, N Qiu… - Precambrian …, 2023 - Elsevier
Manganese-rich deposits in the lower member of the Datangpo Formation (DTP)(ca. 663– 654 Ma) in South China formed in the aftermath of the Cryogenian Sturtian glaciation. The …
J Parnell, C Brolly, AJ Boyce - Geological Magazine, 2021 - cambridge.org
The episode of widespread organic carbon deposition marked by peak black shale sedimentation during the Palaeoproterozoic is also reflected in exceptionally abundant …
Abstract The Bundelkhand craton hosts Banded Iron Formation (BIF) bodies within the east– west trending Bundelkhand Tectonic Zone (BTZ). The BIFs near Mauranipur, BTZ, are massif …
Abstract The Luiswishi Cu–Co ore deposit (Haut-Katanga, DR Congo) belongs to the Katanga Copperbelt (KCB), a world-class Cu–Co district. The primary orebodies in the KCB …