Nature Communications (Sep 2021)

Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites

  • S. M. Chernonozhkin,
  • C. González de Vega,
  • N. Artemieva,
  • B. Soens,
  • J. Belza,
  • E. Bolea-Fernandez,
  • M. Van Ginneken,
  • B. P. Glass,
  • L. Folco,
  • M. J. Genge,
  • Ph. Claeys,
  • F. Vanhaecke,
  • S. Goderis

DOI
https://doi.org/10.1038/s41467-021-25819-6
Journal volume & issue
Vol. 12, no. 1
pp. 1 – 12

Abstract

Read online

Fe isotopic composition of the distal ejecta of a terrestrial impact crater records both evaporation and condensation, refining the nature of the isotopic fractionation taking place during hypervelocity impacts in the Solar System.