New chemical, mineralogical and electron-probe data reveal one of the black chondrite inclusions in Cumberland Falls to be a variety bridging the apparent gap between enstatite and olivine-bronzite chondrites. Transitional properties include oxidized iron content,...
CITATION STYLE
Binns, R. A. (1969). A Chondritic Inclusion of Unique Type in the Cumberland Falls Meteorite (pp. 696–704). https://doi.org/10.1007/978-94-010-3411-1_57
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