Properties of chondrules in EL3 chondrites, comparison with EH3 chondrites, and the implications for the formation of enstatite chondrites
Schneider, D. M., Symes, S. J. K., Benoit, P. H., Sears, D. W. G.(2002). Properties of chondrules in EL3 chondrites, comparison with EH3 chondrites, and the implications for the formation of enstatite chondrites. Meteoritics and Planetary Science, 37(10), 1401-1416. https://doi.org/10.1111/j.1945-5100.2002.tb01037.x
Datasets
| number | title | Methods | variables analyzed | ||
|---|---|---|---|---|---|
| 3 | Composition (wt%) of pyroxene, olivine, and mesostasis in EH3 and EL3 chondrules | EMP | SiO2, TOTAL, FeO, MnO, Cr2O3, Al2O3, CaO, Na2O, MgO, TiO2 | ||
| 4 | Bulk composition (wt%) of chondrules in EL3 and EH3 chondrites | EMP | Na2O, Al2O2, TiO2, CaO, MgO, SiO2, Cr2O3, TOTAL, MnO, FeO | ||
| MB-C | MetBase 4064 Compilation | EMP | Cr, Al, Ca, Na, Si, Ti, Fe, Mg, Mn | ||
Methods
| method name | laboratory | method comment | More details are available for the following variables | |
|---|---|---|---|---|
| ELECTRON MICROPROBE | JOHNSON SPACE CENTER | CAMECA SX100, PAP |
