Potassium Isotope Fractionation in Australasian Microtektites: Evidence for Evaporation and Re-Condensation in a Vapor Plume

Details Potassium Isotope Fractionation in Australasian Microtektites: Evidence for Evaporation and Re-Condensation in a Vapor Plume Potassium Isotope Fractionation in Australasian Microtektites: Evidence for Evaporation and Re-Condensation in a Vapor Plume

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005lpi....36.1167h&link_type=abstract

36th Annual Lunar and Planetary Science Conference, March 14-18, 2005, in League City, Texas, abstract no.1167

Physics

1

Scientific paper

Values of delta(41K)(‰) for 13 Australasian microtektites range
from -10.2±0.5 to +14.1±0.5; no such large effects are
seen in tektites. We propose that the isotopic fractionation took place
in a plume, initially hot but rapidly cooling, associated with
microtektite formation.

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