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- W2166929005 abstract "Calcium-aluminium-rich chondrules were found in L-3 (ALH-77015) and LL-3 (ALH-77278) chondrites. They consist of spinel, olivine, fassaite and glassy groundmass enriched in anorthite component. The bulk chemical compositions of the two chondrules are nearly the same and resemble those of the calcium-aluminium-rich inclusions in the carbonaceous chondrites, but the former is more enriched in MgO and SiO2 and depleted in Al2O3 and CaO. The calcium-aluminium-rich chondrules would have been primarily early condensates which existed at the place where the chondrules were formed, and heated up to 1400 °C or higher to have melted and cooled at the rate similar to those for other chondrules, or the products of intensive heating followed by reaction with gas." @default.
- W2166929005 created "2016-06-24" @default.
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- W2166929005 date "1982-06-01" @default.
- W2166929005 modified "2023-10-02" @default.
- W2166929005 title "CALCIUM-ALUMINIUM-RICH CHONDRULES IN THE UNEQUILIBRATED ORDINARY CHONDRITES" @default.
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- W2166929005 doi "https://doi.org/10.1111/j.1945-5100.1982.tb00556.x" @default.
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