I-Xe dating of Allende inclusions - Antiquity and fine structure

Details I-Xe dating of Allende inclusions - Antiquity and fine structure I-Xe dating of Allende inclusions - Antiquity and fine structure

Apr 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980e%26psl..47..211z&link_type=abstract

Earth and Planetary Science Letters, vol. 47, no. 2, Apr. 1980, p. 211-222.

Computer Science

8

Carbonaceous Chondrites, Inclusions, Meteoritic Composition, Radioactive Age Determination, Relic Radiation, Xenon, Chemical Evolution, Fine Structure, Isotopes, Minerals, Refractory Materials, Thermodynamic Properties, Meteorites, Allende Meteorite, Inclusions, Dating Techniques, Iodine/Xenon, Structure, Isochrons, Ages, Formation, Minerals, Cooling Rate, Thermodynamics, Models, Data, Isotopes, Analysis, Experiments, Temperatures, Composition, St. Severin Meteorite, Comparisons, Chronology, Procedure

Scientific paper

Two inclusions from the Allende meteorite exhibit multiple I-Xe isochrons corresponding to an age difference of 3.7 + or - 1.5 m.y. for their constituent minerals. Consequently, I-Xe dating can establish, independently of thermodynamic models, a partial sequence of formation for minerals that incorporated radioactive I-1290. Additionally, the results give an estimate of the cooling rate for the solar nebula when validity of thermodynamic models is assumed.

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