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Slab melting as a barrier to deep carbon subduction
Interactions between crustal and mantle reservoirs dominate the surface inventory of volatile
elements over geological time, moderating atmospheric composition and maintaining a life …
elements over geological time, moderating atmospheric composition and maintaining a life …
Ce and Eu anomalies in zircon as proxies for the oxidation state of magmas
Chondrite normalized rare earth element (REE) patterns of zircons generally have enriched
Ce values relative to La and Pr, and depleted Eu values relative to Sm and Gd. High Ce …
Ce values relative to La and Pr, and depleted Eu values relative to Sm and Gd. High Ce …
TitaniQ under pressure: the effect of pressure and temperature on the solubility of Ti in quartz
Quartz and rutile were synthesized from silica-saturated aqueous fluids between 5 and 20
kbar and from 700 to 940° C in a piston-cylinder apparatus to explore the potential pressure …
kbar and from 700 to 940° C in a piston-cylinder apparatus to explore the potential pressure …
A diamond-bearing core-mantle boundary on Mercury
Abundant carbon was identified on Mercury by MESSENGER, which is interpreted as the
remnant of a primordial graphite flotation crust, suggesting that the magma ocean and core …
remnant of a primordial graphite flotation crust, suggesting that the magma ocean and core …
The influence of H2O on mantle wedge melting
The solidus and near-solidus melting behavior of a primitive undepleted peridotite
composition has been determined over a pressure range of 1.2–3.2 GPa at H2O saturated …
composition has been determined over a pressure range of 1.2–3.2 GPa at H2O saturated …
Isotope fractionation by chemical diffusion between molten basalt and rhyolite
Experimental diffusion couples were used to study chemical diffusion between molten
rhyolite and basalt with special emphasis on the associated fractionation of calcium and …
rhyolite and basalt with special emphasis on the associated fractionation of calcium and …
Isotope tracers of core formation
The study of siderophile element isotope compositions in planetary mantles offers a new
methodology to constrain the temperatures of core formation, provided there is an …
methodology to constrain the temperatures of core formation, provided there is an …
The beginnings of hydrous mantle wedge melting
This study presents new phase equilibrium data on primitive mantle peridotite (0.33 wt% Na
2 O, 0.03 wt% K 2 O) in the presence of excess H 2 O (14.5 wt% H 2 O) from 740 to 1,200° C …
2 O, 0.03 wt% K 2 O) in the presence of excess H 2 O (14.5 wt% H 2 O) from 740 to 1,200° C …
Magnesium isotope fractionation in silicate melts by chemical and thermal diffusion
FM Richter, EB Watson, RA Mendybaev… - … et Cosmochimica Acta, 2008 - Elsevier
Two types of laboratory experiments were used to quantify magnesium isotopic
fractionations associated with chemical and thermal (Soret) diffusion in silicate liquids …
fractionations associated with chemical and thermal (Soret) diffusion in silicate liquids …
Non-traditional fractionation of non-traditional isotopes: evaporation, chemical diffusion and Soret diffusion
Recent developments documenting high temperature isotope fractionations of a variety of
elements (Li, Mg, Si, Ca, Fe, Ni) by a variety of processes (evaporation, chemical diffusion …
elements (Li, Mg, Si, Ca, Fe, Ni) by a variety of processes (evaporation, chemical diffusion …