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[HTML][HTML] A review of the genesis of the world class Bayan Obo Fe–REE–Nb deposits, Inner Mongolia, China: Multistage processes and outstanding questions
MP Smith, LS Campbell, J Kynicky - Ore Geology Reviews, 2015 - Elsevier
Abstract The Bayan Obo Fe–REE–Nb deposit is the world's largest rare earth element (REE)
resource and with the increasing focus on critical metal resources has become a focus of …
resource and with the increasing focus on critical metal resources has become a focus of …
[HTML][HTML] REE minerals at the Songwe Hill carbonatite, Malawi: HREE-enrichment in late-stage apatite
S Broom-Fendley, AE Brady, F Wall, G Gunn… - Ore Geology …, 2017 - Elsevier
Compared to all published data from carbonatites and granitoids, the fluorapatite
compositions in the Songwe Hill carbonatite, determined by EPMA and LA ICP-MS, have the …
compositions in the Songwe Hill carbonatite, determined by EPMA and LA ICP-MS, have the …
Formation of rare earth deposits in carbonatites
M Anenburg, S Broom-Fendley… - Elements: An …, 2021 - pubs.geoscienceworld.org
Carbonatites and related rocks are the premier source for light rare earth element (LREE)
deposits. Here, we outline an ore formation model for LREE-mineralised carbonatites …
deposits. Here, we outline an ore formation model for LREE-mineralised carbonatites …
Rare earth element mobility in and around carbonatites controlled by sodium, potassium, and silica
Carbonatites and associated rocks are the main source of rare earth elements (REEs),
metals essential to modern technologies. REE mineralization occurs in hydrothermal …
metals essential to modern technologies. REE mineralization occurs in hydrothermal …
Rare earth mineralization in igneous rocks: sources and processes
AR Chakhmouradian, AN Zaitsev - Elements, 2012 - pubs.geoscienceworld.org
Deposits of rare earth elements (REEs) in igneous rocks have played an instrumental role in
meeting the growing industrial demand for these elements since the 1960s. Among the …
meeting the growing industrial demand for these elements since the 1960s. Among the …
A synthesis of mineralization styles with an integrated genetic model of carbonatite-syenite-hosted REE deposits in the Cenozoic Mianning-Dechang REE …
Y Liu, Z Hou - Journal of Asian Earth Sciences, 2017 - Elsevier
Abstract The Cenozoic Mianning–Dechang (MD) rare earth element (REE) belt in eastern
Tibet is an important source of light REE in southwest China. The belt is 270 km long and 15 …
Tibet is an important source of light REE in southwest China. The belt is 270 km long and 15 …
[HTML][HTML] Evolution of rare-earth mineralization in the Bear Lodge carbonatite, Wyoming: Mineralogical and isotopic evidence
M Moore, AR Chakhmouradian, AN Mariano… - Ore Geology Reviews, 2015 - Elsevier
Abstract The Bear Lodge alkaline complex in northeastern Wyoming (USA) is host to
potentially economic rare-earth mineralization in carbonatite and carbonatite-related veins …
potentially economic rare-earth mineralization in carbonatite and carbonatite-related veins …
Experimental evidence reveals the mobilization and mineralization processes of rare earth elements in carbonatites
X Yuan, Z Yang, RA Mayanovic, Z Hou - Science Advances, 2024 - science.org
Whereas the genesis of carbonatitic rare earth element (REE) deposits has long been a
focus of study, the controls on mobilization and mineralization of REEs during magmatic …
focus of study, the controls on mobilization and mineralization of REEs during magmatic …
Multi-stage formation of REE minerals in the Palabora Carbonatite Complex, South Africa
R Johannes Giebel, CDK Gauert, MAW Marks… - American …, 2017 - degruyter.com
Abstract The 2060 Ma old Palabora Carbonatite Complex (PCC), South Africa, comprises
diverse REE mineral assemblages formed during different stages and reflects an …
diverse REE mineral assemblages formed during different stages and reflects an …
Transition from carbonatitic magmas to hydrothermal brines: Continuous dilution or fluid exsolution?
X Yuan, R Zhong, X **ong, J Gao, Y Ma - Science Advances, 2023 - science.org
Carbonatites are the most important primary sources for the rare earth elements (REEs).
While fractional crystallization of carbonate minerals results in the enrichment of volatiles …
While fractional crystallization of carbonate minerals results in the enrichment of volatiles …