I-Xe Ages and the Thermal History of the Toluca IAB Meteorite

Astronomy and Astrophysics – Astrophysics

Scientific paper

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Scientific paper

The I-Xe system in Toluca silicates seems to survive catastrophic impact
and breakup of the IAB parent body. As a result of cooling at about 40
+/- 20 K/Ma, the I-Xe system in the high-Mg pyroxenes in Toluca nodules
closed at about 4559.7 Ma, in low-Mg pyroxenes at 4553.6-4548.9 Ma.

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