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Hydrothermal transport, deposition, and fractionation of the REE: Experimental data and thermodynamic calculations
For many years, our understanding of the behavior of the REE in hydrothermal systems was
based on semi-empirical estimates involving extrapolation of thermodynamic data obtained …
based on semi-empirical estimates involving extrapolation of thermodynamic data obtained …
A review of the coordination chemistry of hydrothermal systems, or do coordination changes make ore deposits?
The hydration and complexation of metals in hydrothermal fluids are key processes
controlling the mobility of elements in the Earth's crust, leading to the formation of ore …
controlling the mobility of elements in the Earth's crust, leading to the formation of ore …
An experimental study of the solubility and speciation of the Rare Earth Elements (III) in fluoride-and chloride-bearing aqueous solutions at temperatures up to 300 C
The solubility of REE (III) fluoride solids was determined in fluoride-and chloride-bearing
solutions at 150, 200 and 250° C and saturated water vapor pressure. These experimental …
solutions at 150, 200 and 250° C and saturated water vapor pressure. These experimental …
Hydrothermal transport and deposition of the rare earth elements by fluorine-bearing aqueous liquids
New technologies, particularly those designed to address environmental concerns, have
created a great demand for the rare earth elements (REE), and focused considerable …
created a great demand for the rare earth elements (REE), and focused considerable …
[PDF][PDF] 13.2–The chemistry of metal transport and deposition by ore-forming hydrothermal fluids
Economically exploitable deposits of metallic minerals (ore deposits) form in the Earth's crust
through a variety of geologic processes. These involve extraction of metals at low …
through a variety of geologic processes. These involve extraction of metals at low …
Multiple stages of hydrothermal REE remobilization recorded in fluorapatite in the Paleoproterozoic Yinachang Fe–Cu–(REE) deposit, Southwest China
The Yinachang deposit in the Kangdian region, Southwest China, contains large amounts of
Fe, Cu and REE, and formed at∼ 1700 Ma. In this deposit, there are three stages of …
Fe, Cu and REE, and formed at∼ 1700 Ma. In this deposit, there are three stages of …
[HTML][HTML] Unraveling rare earth element signatures in hydrothermal carbonate minerals using a source–sink system
Rare earth element and yttrium (REEY) signatures in hydrothermal carbonate minerals are
widely used proxies for studying hydrothermal mineralization. This review adopts a source …
widely used proxies for studying hydrothermal mineralization. This review adopts a source …
A petrogenetic model for the comagmatic origin of chassignites and nakhlites: Inferences from chlorine‐rich minerals, petrology, and geochemistry
Twelve samples belonging to the chassignite and nakhlite subgroups of Martian meteorites
were investigated using a variety of micro‐beam analytical techniques to gain insight into …
were investigated using a variety of micro‐beam analytical techniques to gain insight into …
Experimental investigation into the disturbance of the Sm-Nd isotopic system during metasomatic alteration of apatite
In order to understand the effect of fluid-induced alteration on the Sm-Nd isotope systematic
in apatite, a series of fluid/apatite reaction experiments, which involve reacting the well …
in apatite, a series of fluid/apatite reaction experiments, which involve reacting the well …
Efficient mobilization and fractionation of rare-earth elements by aqueous fluids upon slab dehydration
The characteristic REE fractionation pattern in arc magmas compared to MOR-basalts
results from the selective mobilization of light rare-earth elements (LREE) by slab-derived …
results from the selective mobilization of light rare-earth elements (LREE) by slab-derived …