Chemical studies of H chondrites - 9: Volatile trace element composition and petrographic classification of equilibrated H chondrites

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To examine the thermal history of the parent(s) of equilibrated H chondrites, we treated data for 11 volatile trace elements (Co, Rb, Ag, Se, Cs, Te, Zn, Cd, Bi, Tl, and In in order of putative volatility) in 90 falls: 15 H4; 46 H5, and 29 H6. Using univariate statistical tests, contents of few of these elements differ significantly between any two of these suites. One element, Cs, differs systematically between all 3 pairs of suites: Co and Tl differ between 2 pairs of suites. For Co and Cs, contents varied as H4>H5>H6 while for Tl, H4600 K, with the suites deriving from a stratified parent object(s).

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