“…Coupled 142 Nd-143 Nd isotope systematics have also been used in a variety of materials to determine the differentiation timescales and evolution of terrestrial bodies in the first several hundred million years of the solar system history (e.g. Nyquist et al, 1995;Harper et al, 1995;Borg et al, 1999;Caro et al, 2003;Foley et al, 2005;Boyet and Carlson, 2005;Andreasen and Sharma, 2006;Caro et al, 2006;Rankenburg et al, 2007;Debaille et al, 2007;Bennett et al, 2007;Boyet and Carlson, 2007;Caro et al, 2008). These studies have documented that early differentiation leading to Sm/ Nd ratios that are fractionated relative to average chondrites did occur during in the earliest histories of Earth, Mars, Moon, and the Eucrite Parent Body.…”