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 …
Supercritical fluids at subduction zones: Evidence, formation condition, and physicochemical properties
There is a general consensus that at subduction zones, mass transfer from the subducted
slab to the overlying mantle wedge is mediated by a hydrous mobile phase. However, it is …
slab to the overlying mantle wedge is mediated by a hydrous mobile phase. However, it is …
Carbonate complexation enhances hydrothermal transport of rare earth elements in alkaline fluids
Rare earth elements (REE), essential metals for the transition to a zero-emission economy,
are mostly extracted from REE-fluorcarbonate minerals in deposits associated with …
are mostly extracted from REE-fluorcarbonate minerals in deposits associated with …
Extended Deep Earth Water Model for predicting major element mantle metasomatism
F Huang, DA Sverjensky - Geochimica et Cosmochimica Acta, 2019 - Elsevier
Fluids in the deep crust and upper mantle appear to have played roles in the long-term
evolution of the subcratonic lithospheric mantle and the stabilities of the continents, in the …
evolution of the subcratonic lithospheric mantle and the stabilities of the continents, in the …
Channelized fluid flow and eclogite-facies metasomatism along the subduction shear zone
Abstract The Monviso ophiolite Lago Superiore Unit (LSU; Western Alps) constitutes a well-
preserved, largely coherent fragment of eclogitic upper oceanic lithosphere subducted to c …
preserved, largely coherent fragment of eclogitic upper oceanic lithosphere subducted to c …
Extreme Zr stable isotope fractionation during magmatic fractional crystallization
M Ibañez-Mejia, FLH Tissot - Science Advances, 2019 - science.org
Zirconium is a commonly used elemental tracer of silicate differentiation, yet its stable
isotope systematics remain poorly known. Accessory phases rich in Zr4+ such as zircon and …
isotope systematics remain poorly known. Accessory phases rich in Zr4+ such as zircon and …
Drivers of zirconium isotope fractionation in Zr-bearing phases and melts: the roles of vibrational, nuclear field shift and diffusive effects
Conflicting results exist regarding the mechanisms, direction, and magnitude of Zr isotope
fractionation in igneous systems. To better understand the origin of the fractionations …
fractionation in igneous systems. To better understand the origin of the fractionations …
Magmatic crystallization drives zircon Zr isotopic variations in a large granite batholith
Stable zirconium (Zr) isotope of magmatic zircons is a promising new tracer to understand
magma differentiation in the continental crust. However, magmatic processes controlling …
magma differentiation in the continental crust. However, magmatic processes controlling …
Zirconium and its stable isotopes in igneous systems
Zirconium, as a high field strength element, has been widely used to trace the differentiation
of terrestrial planets. It is also a major constituent in zircon, an important accessory mineral …
of terrestrial planets. It is also a major constituent in zircon, an important accessory mineral …
Stable zirconium isotopic fractionation during alkaline magma differentiation: Implications for the differentiation of continental crust
Stable Zr isotopes have shown great potential in tracing magma differentiation. However, it
remains unclear if different magmatic systems have similar Zr isotopic evolution patterns …
remains unclear if different magmatic systems have similar Zr isotopic evolution patterns …