«One of the assumptions being made is that
the composition of the zircons and the rocks in which they have formed give an accurate record of the magmas and conditions at which the zircons and magmas formed,» Associate Professor Bryan said.
Working with Miller and doctoral student Abraham Padilla at Vanderbilt, Joe Wooden at Stanford University, Axel Schmitt and Rita Economos from UCLA, Ilya Bindeman at the University
of Oregon and Brennan Jordan at the University
of South Dakota, Carley analyzed about 1,000
zircon crystals for their age and elemental and isotopic
compositions.