Cosmic-ray produced nuclear tracks and noble gases have been studied i
n the martian orthopyroxenite Allan Hills 84001 to delineate its cosmi
c-ray exposure history, preatmospheric size, and fall characteristics.
A K-Ar age of 3.9 Ga, cosmic-ray exposure duration of 16.7 Ma, and a
preatmospheric radius of 10 cm have been deduced from the noble gas an
d track data. The track data suggest ALH 84001 to be a single fall tha
t has suffered atmospheric mass ablation in excess of 85%, higher than
the value deduced for the shergottites, ALHA 77005, EETA 79001, and S
hergotty. The formation age, as well as the cosmic-ray exposure durati
on, determined in this work are in good agreement with values reported
earlier and are distinctly different from other shergottite, nakhlite
, and chassignite (SNC) meteorites analysed so far. The high cosmogeni
c Ne-22/Ne-21 ratio of 1.22 most probably reflects an effect due to no
n-chondritic composition of ALH 84001 as the track data suggest high s
hielding (greater than or equal to 5cm) for the analysed samples. Ther
e are signatures in the noble gas data that indicate the possible pres
ence of trapped Ar and Ne of martian atmospheric origin in ALH 84001.