Controls on REE mineralization in the Tioueine ring complex (Western Hoggar, Algeria): examination of magmatic vs hydrothermal processes
Rattachement africain : ca, Algérie. Niveau de preuve : code pays fourni par la source.
Le résumé fourni par la source
The Hoggar is a rare metal endowed province within the Tuareg shield with variably mineralized post Pan-African granitoid complexes. The investigated Tioueine Ring Complex is among them, with two major units: a weakly evolved calc-alkaline central unit containing monzogranite and granodiorite, and a highly evolved alkali feldspar granite-dominated major outer unit that hosts magmatic to magmatic-hydrothermal LREE-dominant mineralization. The Tioueine Ring Complex is a mantle-derived A 1 -type granitoid complex that crystallized at ca. 600 Ma during a post-orogenic to anorogenic episode of the Pan-African orogeny. Its parental magmatic system is characterized by high concentrations of alkali elements, with moderate total REE 2 O 3 (TREE 2 O 3 ) contents up to 0.2 wt%; allanite is the major REE-rich mineral, with limited proportions of apatite, xenotime, and rare monazite. Primary mineralization resulted from low degrees of partial melting of an enriched mantle source that produced reduced ferroan REE-rich magma following advective mantle heat input. The derivative melt may have experienced crustal assimilation and crystal fractionation that caused further enrichment in HFSE and REE before reaching the solidus. A late- to post-magmatic-hydrothermal event allowed limited secondary enrichment of REE by causing allanite breakdown to form REE-fluorocarbonate minerals. Fluid—rock interaction likely resulted from magmatic-hydrothermal F- and CO 2 -rich aqueous fluids and late meteoric hydrothermal fluids that circulated through ring faults. The Tioueine Ring Complex exhibits elevated REE concentrations that warrant follow-up sampling and drilling to assess its economic viability. However, despite REE enrichment in A-type granites globally, the role of F-rich fluids in remobilizing REE from magmatic allanite to form hydrothermal REE-fluorocarbonates remains poorly constrained. The Tioueine Ring Complex offers a case study to elucidate this process.
Ce résumé expose les affirmations des auteurs. BNTIC ne l’interprète pas comme une validation indépendante des résultats.
Le contrôle bibliographique ouvert
DOI retrouvé dans Crossref DOI retrouvé ; titre concordant.
- Titre Crossref
- Controls on REE mineralization in the Tioueine ring complex (Western Hoggar, Algeria): examination of magmatic vs hydrothermal processes
- Date Crossref
- 01/01/2026
- Éditeur
- Elsevier BV
- Type
- journal-article
Ce recoupement confirme des métadonnées liées au DOI. Il ne confirme ni la méthode ni les conclusions de l’étude, et il ne compte pas comme une seconde source scientifique indépendante.
Les institutions déclarées
Une affiliation ne permet pas de déduire la nationalité d’un auteur.