Abstract
Summary
Large samples of the hexahedrites
Scottsville, Indian Valley, Okano, Puripica, and
Hex River Mountains from the British Museum
Collection and a sample of Lombard have been
prepared for metallographic examination and
details of their structures have been mapped with
the aid of a specially constructed
X-Y plotting device
that is geared to the stage of a metallurgical
microscope. The following elements of structure
have been studied and an attempt has been made to
discuss the circumstances under which they were
formed: clear etching and frosty etching kamacite,
decorated Neumann lines, giant rhabdites, plate
rhabdites, rhabdite clusters, microrhabdites,
cohenite or decomposed cohenite, and troilite
(which in some instances is recrystallized or
remelted). In general the range of structural
effects is similar to that previously reported for
the Angra dos Reis hexahedrite (Min. Mag. 1971,
38, 94–101). The variations
of structure are discussed in relation to nickel
content and trace element chemistry of the
meteorites.
Subject
Geochemistry and Petrology
Cited by
7 articles.
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