Petrology and origin of amoeboid olivine aggregates in CR chondrites
Weisberg, Michael K., Connolly, Harold C., Ebel, Denton S.(2004). Petrology and origin of amoeboid olivine aggregates in CR chondrites. Meteoritics & Planetary Science, 39(10). https://doi.org/10.1111/j.1945-5100.2004.tb00070.x
Datasets
| number | title | Methods | variables analyzed | ||
|---|---|---|---|---|---|
| 1 | Representative analyses (wt%) of olivine in AOAs in CR chondrites | SiO2, Cr2O3, FeO, MnO, MgO, CaO, TOTAL, FAYALITE | |||
| 2 | Representative analyses (wt%) of refractory phases in AOAs in CR chondrites | SiO2, TiO2, Al2O3, Cr2O3, FeO, MnO, MgO, CaO, TOTAL | |||
| 3 | Representative analyses (wt%) of minerals in the EET92-21 type A inclusion core, Wark-Lovering rim, and the AOA attached to the rim | SiO2, TiO2, Al2O3, Cr2O3, FeO, MgO, CaO, TOTAL | |||
Methods
| method name | laboratory | method comment | More details are available for the following variables | |
|---|---|---|---|---|
| ELECTRON MICROPROBE | UNKNOWN | Cameca SX100; data reduction Pouchou and Pichoir (1991) |
