Zoning patterns of trace elements (TE) in minerals from Ca-, Al-rich inclusions (CAIs) may reflect how they formed [1] and/or yield information on secondary processes. We have measured abundances of the REE, Ba, Be, Sc and Ti in a single melilite (Mel) crystal (Xl) from the mantle of the Allende type B 1 inclusion Egg-6 [2] and in the rim of a coexisting clinopyroxene (CPX) at the core/mantle interface. TE zoning profiles in Mel from Egg-6 are compared with those predicted by [1] for fractional crystallization of Mel in type B CAIs
Small (<5 μm) boundary clinopyroxenes (b-cpx) on spinel (sp) inclusions in melilite (mel) are ubiqu...
The measurements of magnesium and potassium isotopic compositions of refractory minerals in Allende ...
Ca, Al-rich inclusions (CAIs) often contain numerous refractory metal nuggets (RMNs), consisting of ...
Zoning patterns of trace elements (TE) in minerals from Ca-, Al-rich inclusions (CAIs) may reflect ...
Variations in refractory major and trace element composition of calcium, aluminum-rich inclusions (C...
Concentrations of refractory lithophile elements (RLEs) in Type B1 Ca-Al-rich inclusions (CAIs) are ...
Of the possible processes involved in Type B CAI history, igneous processes are the most tractable f...
We have shown [1-3] that the variation in the minor-element concentration of spinels (MgAI_20_4 and ...
The trace element chemistry of CAi's is complicated because of their multistage histories (e.g., Gro...
We have conducted an electron microprobe study of minor element distributions among spinels from two...
The partitioning behavior of the trace elements Be, Sc, Ba, La, Ce, and Tm between melilite and liqu...
Ca-Al-rich inclusions (CAIs) are the earliest formed crystalline material in our solar system and th...
Calcium-aluminum-rich inclusions (CAIs) are the key to understanding physical and chemical condition...
of the refractory elements are enriched by a mean factor of 18.6 relative to their concentrations in...
Minor element variations in MgAl_2O_4 spinel from the type B1 calcium-aluminum-rich inclusion (CAI) ...
Small (<5 μm) boundary clinopyroxenes (b-cpx) on spinel (sp) inclusions in melilite (mel) are ubiqu...
The measurements of magnesium and potassium isotopic compositions of refractory minerals in Allende ...
Ca, Al-rich inclusions (CAIs) often contain numerous refractory metal nuggets (RMNs), consisting of ...
Zoning patterns of trace elements (TE) in minerals from Ca-, Al-rich inclusions (CAIs) may reflect ...
Variations in refractory major and trace element composition of calcium, aluminum-rich inclusions (C...
Concentrations of refractory lithophile elements (RLEs) in Type B1 Ca-Al-rich inclusions (CAIs) are ...
Of the possible processes involved in Type B CAI history, igneous processes are the most tractable f...
We have shown [1-3] that the variation in the minor-element concentration of spinels (MgAI_20_4 and ...
The trace element chemistry of CAi's is complicated because of their multistage histories (e.g., Gro...
We have conducted an electron microprobe study of minor element distributions among spinels from two...
The partitioning behavior of the trace elements Be, Sc, Ba, La, Ce, and Tm between melilite and liqu...
Ca-Al-rich inclusions (CAIs) are the earliest formed crystalline material in our solar system and th...
Calcium-aluminum-rich inclusions (CAIs) are the key to understanding physical and chemical condition...
of the refractory elements are enriched by a mean factor of 18.6 relative to their concentrations in...
Minor element variations in MgAl_2O_4 spinel from the type B1 calcium-aluminum-rich inclusion (CAI) ...
Small (<5 μm) boundary clinopyroxenes (b-cpx) on spinel (sp) inclusions in melilite (mel) are ubiqu...
The measurements of magnesium and potassium isotopic compositions of refractory minerals in Allende ...
Ca, Al-rich inclusions (CAIs) often contain numerous refractory metal nuggets (RMNs), consisting of ...