Partial melting, fluid supercriticality and element mobility in ultrahigh-pressure metamorphic rocks during continental collision

YF Zheng, QX **a, RX Chen, XY Gao - Earth-Science Reviews, 2011 - Elsevier
Partial melting at continental lithosphere depths plays an important role in generating
geochemical variations in igneous rocks. In particular, dehydration melting of ultrahigh …

An H2O–CO2 mixed fluid saturation model compatible with rhyolite-MELTS

MS Ghiorso, GAR Gualda - Contributions to Mineralogy and Petrology, 2015 - Springer
A thermodynamic model for estimating the saturation conditions of H 2 O–CO 2 mixed fluids
in multicomponent silicate liquids is described. The model extends the capabilities of rhyolite …

Thermodynamic model for uplift and deflation episodes (bradyseism) associated with magmatic–hydrothermal activity at the Campi Flegrei (Italy)

A Lima, B De Vivo, FJ Spera, RJ Bodnar, A Milia… - Earth-Science …, 2009 - Elsevier
Campi Flegrei (CF) is a large volcanic complex located west of the city of Naples, Italy.
Repeated episodes of bradyseism (slow vertical ground movement) near the town of …

Fluid fractionation of tungsten during granite–pegmatite differentiation and the metal source of peribatholitic W quartz veins: Evidence from the Karagwe-Ankole Belt …

N Hulsbosch, MC Boiron, S Dewaele… - … et Cosmochimica Acta, 2016 - Elsevier
The identification of a magmatic source for granite-associated rare metal (W, Nb, Ta and Sn)
mineralisation in metasediment-hosted quartz veins is often obscured by intense fluid–rock …

Magmatic fractionation and the magmatic-hydrothermal transition in rare metal granites: Evidence from Argemela (Central Portugal)

JAS Michaud, M Pichavant - Geochimica et Cosmochimica Acta, 2020 - Elsevier
Abstract Rare Metal Granites (RMGs) are highly evolved intrusions with specific
geochemical signatures that are the result of combined magmatic and hydrothermal …

Rare-metal enrichment and Nb–Ta fractionation during magmatic–hydrothermal processes in rare-metal granites: Evidence from zoned micas from the Yashan pluton …

R Yin, XL Huang, RC Wang, XM Sun, Y Tang… - Journal of …, 2022 - academic.oup.com
Rare-metal mineralization in aluminous granites (ie rare-metal granites, RMGs) is usually
associated with high degree of magma fractionation, strong enrichment in fluxing elements …

Diagnosing open-system magmatic processes using the Magma Chamber Simulator (MCS): part II—trace elements and isotopes

JS Heinonen, WA Bohrson, FJ Spera, GA Brown… - … to Mineralogy and …, 2020 - Springer
Abstract The Magma Chamber Simulator (MCS) is a thermodynamic model that computes
the phase, thermal, and compositional evolution of a multiphase–multicomponent system of …

The origin of trachyte and pantellerite from Pantelleria, Italy: insights from major element, trace element, and thermodynamic modelling

JC White, DF Parker, M Ren - Journal of Volcanology and Geothermal …, 2009 - Elsevier
Trachyte and peralkaline rhyolite (pantellerite and comendite) frequently comprise the felsic
end-member in bimodal suites in continental rift and oceanic island settings. In these …

Thermodynamic model for energy-constrained open-system evolution of crustal magma bodies undergoing simultaneous recharge, assimilation and crystallization …

WA Bohrson, FJ Spera, MS Ghiorso… - Journal of …, 2014 - academic.oup.com
The Magma Chamber Simulator quantifies the impact of simultaneous recharge,
assimilation and crystallization through mass and enthalpy balance in a multicomponent …

Trace elements in zircon and coexisting minerals from low-T/UHP metagranite in the Dabie orogen: implications for action of supercritical fluid during continental …

QX **a, YF Zheng, Z Hu - Lithos, 2010 - Elsevier
Simultaneously in-situ analyses of U–Pb isotopes and trace elements were carried out for
zircons, in combination with the in-situ analyses of trace elements in coexisting minerals …