The formation age of the Brachina meteorite

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Achondrites, Geochronology, Nuclear Particles, Particle Tracks, Asteroids, Calcium Phosphates, Cosmic Rays, Plutonium Isotopes

Scientific paper

The Brachina meteorite, which was until recently classified as a chassignite, is presently subjected to a nuclear particle track study of its various phases. Detected fission tracks that are due to the decay of Pu-244, whose T(1/2) is 82 million years, indicate that Brachina formed about 4.5 billion years ago in a parent body which was probably asteroidal in size. On the basis of the present results and of evidence independently adduced by other researchers, it is concluded that there is no need to postulate a Martian origin for this meteorite.

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