Results 141 to 150 of about 7,282 (216)
Some of the next articles are maybe not open access.

Related searches:

Significance of hydrothermal reworking for REE mineralization associated with carbonatite: Constraints from in situ trace element and C-Sr isotope study of calcite and apatite from the Miaoya carbonatite complex (China)

Geochimica Et Cosmochimica Acta, 2020
A majority of carbonatite-related rare earth element (REE) deposits are found in cratonic margins and orogenic belts, and metasomatic/hydrothermal reworking is common in these deposits; however, the role of metasomatic processes involved in their ...
Yuan-Can Ying   +2 more
exaly   +2 more sources

The Carbonatite-Related Morro do Padre Niobium Deposit, Catalão II Complex, Central Brazil

Economic Geology, 2022
The Morro do Padre deposit contains a valuable niobium resource estimated at 14.5 Mt at 1.52 wt % Nb2O5 (at a cut-off grade of 0.5% Nb2O5) hosted in carbonatite-related rocks and their regolith in the southern part of the Catalão II Complex, in central
M. Palmieri   +10 more
semanticscholar   +1 more source

Mineralogical and Geochemical Evidence of Dissolution-Reprecipitation Controlled Hydrothermal Rare Earth Element Mineralization in the Amba Dongar Carbonatite Complex, Gujarat, Western India

Economic Geology, 2022
The Amba Dongar carbonatite complex in western India comprises an inner ring of carbonatite breccia surrounded by a sövite ring dike. The various carbonatite units in the body include calcite carbonatite, alvikite, dolomite carbonatite, and ankerite ...
A. K. Patel   +3 more
semanticscholar   +1 more source

The formation of the giant Huayangchuan U-Nb deposit associated with carbonatite in the Qingling Orogenic Belt

Ore Geology Reviews, 2020
Carbonatitic magmatism plays a significant role in outgassing carbon from mantle and the formation of rare earth element (REE), rare metal (e.g., Nb and Th) and other types of deposits. The mechanism of REE mineralization associated with carbonatite have
Ming-Xing Ling, Weidong Sun, Yu-Long Liu
exaly   +2 more sources

Fluids associated with carbonatitic magmatism: A critical review and implications for carbonatite magma ascent

, 2021
Carbonatites are formed from volatile-rich melts, commonly associated with a characteristic hydrothermal footprint. However, studies of their fluid inclusions are relatively scarce and heterogeneous in terms of detail and completeness of the data ...
B. Walter   +5 more
semanticscholar   +1 more source

The role of sulfate-, alkali-, and halogen-rich fluids in mobilization and mineralization of rare earth elements: Insights from bulk fluid compositions in the Mianning–Dechang carbonatite-related REE belt, southwestern China

, 2021
Carbonatites host the world's most important rare earth element (REE) resources. The origins of REE mineralization in carbonatite-related deposits, particularly the role of hydrothermal fluids in REE mobilization and mineralization, remain enigmatic. The
Xu Zheng, Yan Liu, Liang Zhang
semanticscholar   +1 more source

Fenites associated with carbonatite complexes: A review

open access: yesOre Geology Reviews, 2018
This research has received funding from the European Union’s Horizon 2020 research and innovation programme under grant No 689909.
Frances Wall, Samuel M. Weatherley
exaly   +2 more sources

Hydrothermal alteration of pyrochlore group minerals from the Miaoya carbonatite complex, central China and its implications for Nb mineralization

, 2021
Carbonatite represents a major host rock for niobium (Nb) resources worldwide. Both magmatic and post-magmatic metasomatic processes are crucial for Nb mineralization in carbonatites.
Bin Wu   +7 more
semanticscholar   +1 more source

Fingerprinting REE mineralization and hydrothermal remobilization history of the carbonatite-alkaline complexes, Central China: Constraints from in situ elemental and isotopic analyses of phosphate minerals

American Mineralogist, 2021
Carbonatites and related alkaline rocks host most REE resources. Phosphate minerals, e.g., apatite and monazite, commonly occur as the main REE-host in carbonatites and have been used for tracing magmatic and mineralization processes.
Jian-Hui Su   +6 more
semanticscholar   +1 more source

Home - About - Disclaimer - Privacy