Add to ORKGExperimental data are reported on Mg diffusion in plagioclase crystals with a range of anorthite conten
Significant amounts of iron, magnesium and Na (and/or Ca) vacancy are found in meteoritic plagioclas...
With a half-life of 0.73 Myr, the 26Al-to-26Mg decay system is the most widely used short-lived chro...
Discerning crystal growth from olivine by in situ Mg–F between melt and olivine. The data can be exp...
We have measured the self diffusion coefficients of Mg, Ca, and Sr in anorthitic plagioclase in orde...
Compilation and interpretation of experimental and natural Nernst partition coefficient (plagioclase...
The isothermal (750°C) experiments of Lagache and Dujon (1987) reveal that the partitioning of Sr be...
We have measured Mg self-diffusion in spinel and coexisting melt at bulk chemical equilibrium using ...
Tracer diffusion kinetics at 1 atm pressure under 'dry ' conditions using 6Li, 41K, and S7...
International audienceThe timing of the formation of the first solids in the solar system remains po...
[1] Plagioclase, the most abundant mineral in many terrestrial and Martian igneous rocks, exhibits a...
The chemical anomalies of meteoritic plagioclase which appear also in lunar plagioclase, result in t...
[[abstract]]The Mg isotopic composition in plagioclase from the Allende inclusion Cl has been measur...
The canonical initial 26Al/27Al ratio of 4.5 x 10-5 has been a fiducial marker for the beginning of ...
SUMMARY. Electron microprobe and textural data are used to deduce a crystallization history for plag...
Trace element partition coefficients between anorthitic plagioclase and basaltic melts (D) have been...
Significant amounts of iron, magnesium and Na (and/or Ca) vacancy are found in meteoritic plagioclas...
With a half-life of 0.73 Myr, the 26Al-to-26Mg decay system is the most widely used short-lived chro...
Discerning crystal growth from olivine by in situ Mg–F between melt and olivine. The data can be exp...
We have measured the self diffusion coefficients of Mg, Ca, and Sr in anorthitic plagioclase in orde...
Compilation and interpretation of experimental and natural Nernst partition coefficient (plagioclase...
The isothermal (750°C) experiments of Lagache and Dujon (1987) reveal that the partitioning of Sr be...
We have measured Mg self-diffusion in spinel and coexisting melt at bulk chemical equilibrium using ...
Tracer diffusion kinetics at 1 atm pressure under 'dry ' conditions using 6Li, 41K, and S7...
International audienceThe timing of the formation of the first solids in the solar system remains po...
[1] Plagioclase, the most abundant mineral in many terrestrial and Martian igneous rocks, exhibits a...
The chemical anomalies of meteoritic plagioclase which appear also in lunar plagioclase, result in t...
[[abstract]]The Mg isotopic composition in plagioclase from the Allende inclusion Cl has been measur...
The canonical initial 26Al/27Al ratio of 4.5 x 10-5 has been a fiducial marker for the beginning of ...
SUMMARY. Electron microprobe and textural data are used to deduce a crystallization history for plag...
Trace element partition coefficients between anorthitic plagioclase and basaltic melts (D) have been...
Significant amounts of iron, magnesium and Na (and/or Ca) vacancy are found in meteoritic plagioclas...
With a half-life of 0.73 Myr, the 26Al-to-26Mg decay system is the most widely used short-lived chro...
Discerning crystal growth from olivine by in situ Mg–F between melt and olivine. The data can be exp...