Copper isotopes in the martian mantle are heavier than those in chondritic precursors, indicating that sulfides extracted isotopically light copper into the core during planetary differentiation. This process resulted in a sulfur-poor mantle and a sulfur-rich core, accounting for the observed depletion of chalcophile elements in the mantle. Isotopic evidence and modeling further reveal the history of martian differentiation, providing new insights into the early evolution of Mars.
- De-Liang Wang
- Dan Zhu
- Jian-Zhong Liu