Testing the Homogeneity of the Solar System for Iron (54, 56, 57, and 58) and Tungsten (182, 183, 184, and 186) Isotope Abundances
The solar nebula was homogenized at a planetary scale at the 0.2 epsilon and 0.5 epsilon level for iron-56 and iron-58, respectively. Preliminary results seem to indicate the presence of a s-process tungsten component in leaching experiments of primitive meteorites.
Lunar and Planetary Science Conference
- Pub Date:
- March 2004