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Mineral-melt partitioning of uranium, thorium and their daughters
The uranium and thorium decay series (hereafter “U-series”) include the nuclides of ten
elements, all of which can be found at trace levels in rocks and minerals. The relatively short …
elements, all of which can be found at trace levels in rocks and minerals. The relatively short …
The effect of Ca-Tschermaks component on trace element partitioning between clinopyroxene and silicate melt
We have studied the influence of Ca-Tschermaks (Calcium Tschermaks or CaTs) content of
clinopyroxene on the partitioning of trace elements between this phase and silicate melt at …
clinopyroxene on the partitioning of trace elements between this phase and silicate melt at …
Experimental comparison of trace element partitioning between clinopyroxene and melt in carbonate and silicate systems, and implications for mantle metasomatism
J Blundy, J Dalton - Contributions to Mineralogy and Petrology, 2000 - Springer
Experiments in the systems diopside-albite (Di-Ab) and diopside-albite-dolomite (Di-Ab-
Dmt), doped with a wide range of trace elements, have been used to characterise the …
Dmt), doped with a wide range of trace elements, have been used to characterise the …
Systematics of calcium partitioning between olivine and silicate melt: implications for melt structure and calcium content of magmatic olivines
G Libourel - Contributions to Mineralogy and Petrology, 1999 - Springer
A systematic characterization of the chemical factors that control calcium partitioning
between olivine and melt in a magmatic environment was undertaken using experiments …
between olivine and melt in a magmatic environment was undertaken using experiments …
Grain boundaries as reservoirs of incompatible elements in the Earth's mantle
T Hiraga, IM Anderson, DL Kohlstedt - Nature, 2004 - nature.com
The concentrations and locations of elements that strongly partition into the fluid phase in
rocks provide essential constraints on geochemical and geodynamical processes in Earth's …
rocks provide essential constraints on geochemical and geodynamical processes in Earth's …
Distinct site preferences for heavy and light REE in amphibole and the prediction of Amph/LDREE
New experimental amphibole/melt partition coefficients from a variety of geologically
relevant amphibole (pargasite, kaersutite, and K-richterite) and melt compositions obtained …
relevant amphibole (pargasite, kaersutite, and K-richterite) and melt compositions obtained …
Modelling the effect of water on the surface structure and stability of forsterite
We describe the application of atomistic simulation techniques to investigate the effect of
associative and dissociative adsorption of water on the structures and stabilities of the low …
associative and dissociative adsorption of water on the structures and stabilities of the low …
Atomistic simulation of trace element incorporation into garnets—comparison with experimental garnet-melt partitioning data
We have studied the energetics of trace element incorporation into pure almandine (Alm),
grossular (Gros), pyrope (Py) and spessartine (Spes) garnets (X3Al2Si3O12, with X= Fe, Ca …
grossular (Gros), pyrope (Py) and spessartine (Spes) garnets (X3Al2Si3O12, with X= Fe, Ca …
Trace element partitioning between phlogopite, clinopyroxene and leucite lamproite melt
KH Schmidt, P Bottazzi, R Vannucci… - Earth and Planetary …, 1999 - Elsevier
Partition coefficients for Rb, Sr, Sm, Nd, U, Th, Pb, La, Ce, Ba, Nb, and Li between
phlogopite, clinopyroxene and melt were determined in order to characterize the effect of …
phlogopite, clinopyroxene and melt were determined in order to characterize the effect of …
Engineering atomic size mismatch in Pr3+, La3+ codoped Lu3Al5O12 garnet single crystals for tailored structure and functional properties
This study provided the first in-depth investigation of the effects of large dopant
incompatibility (Pr 3+ and La 3+ ions) on the small host lattice element (Lu 3+) in Lu 3 Al 5 O …
incompatibility (Pr 3+ and La 3+ ions) on the small host lattice element (Lu 3+) in Lu 3 Al 5 O …