IAD Index of Academic Documents
  • Home Page
  • About
    • About Izmir Academy Association
    • About IAD Index
    • IAD Team
    • IAD Logos and Links
    • Policies
    • Contact
  • Submit A Journal
  • Submit A Conference
  • Submit Paper/Book
    • Submit a Preprint
    • Submit a Book
  • Contact
  • Maden Tetkik ve Arama Dergisi
  • Cilt: 178 Sayı: 178
  • Geochemical and geophysical relationship of the potassium-rich fenite zone in surface and subsurface...

Geochemical and geophysical relationship of the potassium-rich fenite zone in surface and subsurface investigations of the giant Kuluncak (Malatya) Nb-U-REE-Zr-Li mineralization

Authors : Okan Pulat, Murat Kirtil, Mustafa Karakaş, Mustafa Küçük, Ahmet Mert Ulutaş, Murat Akgöz, Ali Tugcan Unluer, Hülya Ateş, Mehmet Burak Omaç, Özkan Türkan
Pages : 149-181
Doi:10.19111/bulletinofmre.1812181
View : 217 | Download : 689
Publication Date : 2025-12-23
Article Type : Research Paper
Abstract :The Kuluncak (Malatya) district hosts one of the most significant Nb–U–REE–Zr–Li mineralizations in Türkiye, spatially associated with alkaline and carbonatite-related rocks. In this study, geochemical and geophysical investigations were integrated with surface and drillhole data to evaluate the role of fenitization in rare earth element enrichment. The drillhole profiles reveal systematic variations: in marble-hosted sections, light rare earth element (LREE) anomalies occur near-surface zones coupled with K2O enrichment, whereas in nepheline syenite-hosted drillholes, REE anomalies are concentrated at intermediate depths (~40–100 m) with heterogeneous distributions. High CaO concentrations, together with fluorite, barite, apatite, and Nb–REE-bearing minerals, confirm a strong carbonatitic contribution. Geophysical anomalies (spectral gamma, magnetic maps) support the geochemical evidence and were used to identify subsurface fenite zones. Comparison with other carbonatite-related systems in Türkiye, such as the Özvatan complex (Kayseri) and Eskişehir, indicates that Kuluncak represents one of the most carbonatite-dominant and LREE-enriched systems in the region. On a global scale, the geochemical features of Kuluncak resemble world-class deposits such as Bayan Obo (China) and Ilímaussaq (Greenland). These findings demonstrate that fenitization and carbonatite-related metasomatism are the principal processes controlling mineralization, highlighting the Kuluncak district as a strategic Nb–REE resource of both national and international importance.
Keywords : Fenite, Rare Earth Elements (REE), Niobium (Nb), Uranium (U), Zirconium (Zr).

ORIGINAL ARTICLE URL

* There may have been changes in the journal, article,conference, book, preprint etc. informations. Therefore, it would be appropriate to follow the information on the official page of the source. The information here is shared for informational purposes. IAD is not responsible for incorrect or missing information.


Index of Academic Documents
İzmir Academy Association
CopyRight © 2023-2026