(Ar-39)-(Ar-40) dating of mesosiderites - Evidence for major parent body disruption less than 4 GA ago

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Argon Isotopes, Models, Radioactive Age Determination, Activation Energy, Degassing, Plutonium Isotopes, Siderites, Silicates, Temperature Dependence

Scientific paper

The (Ar-39) (Ar-40) chronologies were determined for 14 different mesosiderites representing the full range of classification according to recrystallization, and these chronologies were compared with analogous data for other meteorite types and for lunar highland rocks. Results of Ar-Ar chronologies indicate the history of a degassing of Ar due to a major thermal event that occurred less than 3.9 Ga ago; this event is not the metal-silicate mixing event, which is known to have occurred earlier than 4.4 Ga ago. It is suggested that a major collisional disruption-reassembly event less than 3.9 Ga ago took place, leaving the metal-silicate breccias buried under tens of kilometers of rubble, where they cooled slowly through the Ar closure temperatures.

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