Ms. Wang et al., Chemical studies of H chondrites-10: Contents of thermally labile trace elements are unaffected by late heating, METEORIT PL, 34(5), 1999, pp. 713-716
We have used radiochemical neutron activation analysis (RNAA) to determine
15 trace elements, including 10 moderately to highly volatile ones-Rb, Ag,
Se, Cs, Te, Zn, Cd, Bi, Tl, In (in increasing volatility order), in 6 H cho
ndrite falls with low-He-3 contents. These (plus prior RNAA data) provide a
compositional database of 92 H4-6 chondrite falls. Three suites of samples
can be identified from their noble gas contents: 44 with "normal" contents
and, therefore, "normal" orbits and cosmic-ray exposure histories; 8 that
lost radiogenic gases, presumably by shock late in their histories; and 17
that lost cosmogenic gases by heating during close solar approach. We used
the standard multivariate statistical techniques of linear discriminant ana
lysis and logistic regression to compare contents of the 10 moderately and
highly volatile trace elements, listed above, in these three suites. We fou
nd no significant differences. This contrasts sharply with similar comparis
ons involving random falls and H4-6 chondrites that landed on Earth at spec
ific time intervals. Apparently, contents of volatile trace elements in H4-
6 chondrites were established early in their histories, and they are so ret
entively sited that loss during later heating episodes did not occur.