Skip to main content
. Author manuscript; available in PMC: 2020 Dec 2.
Published in final edited form as: Geochim Cosmochim Acta. 2020 Aug 3;288:36–50. doi: 10.1016/j.gca.2020.07.036

Figure 1.

Figure 1.

CI chondrite normalized abundances of siderophile elements for the IIC irons, Wiley and Pará de Minas. Elements are listed in order of decreasing 50% condensation temperatures from left to right. Bulk composition data were normalized to data for CI chondrites (Lodders and Fegley, 1998).