Fused Meteoritic Iron: Second Paper
Identifieur interne : 001975 ( Main/Exploration ); précédent : 001974; suivant : 001976Fused Meteoritic Iron: Second Paper
Auteurs : John Davis Buddhue [États-Unis]Source :
- Contributions of the Society for Research on Meteorites [ 0096-2813 ] ; 1939-01.
Abstract
Specimens of Henbury, Central Australia, and Canyon Diablo, Arizona, were fused and examined metallographically. Henbury gave a fine granular structure with probably nickel‐rich grain boundaries. Canyon Diablo, containing schreibersite, gave a granular structure, except where the schreibersite produced a pearlite‐like mixture. At the edges of this was a structure resembling martensite. Another specimen fused on charcoal was composed partly of grains of ferrite inclosed in cementite. The remainder showed a dendritic structure. This specimen exploded during fusion. Mention is made of other work in this field.
Url:
DOI: 10.1111/j.1945-5100.1939.tb00232.x
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream Istex, to step Corpus: 000425
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- to stream Main, to step Merge: 001A48
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Le document en format XML
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<front><div type="abstract" xml:lang="en">Specimens of Henbury, Central Australia, and Canyon Diablo, Arizona, were fused and examined metallographically. Henbury gave a fine granular structure with probably nickel‐rich grain boundaries. Canyon Diablo, containing schreibersite, gave a granular structure, except where the schreibersite produced a pearlite‐like mixture. At the edges of this was a structure resembling martensite. Another specimen fused on charcoal was composed partly of grains of ferrite inclosed in cementite. The remainder showed a dendritic structure. This specimen exploded during fusion. Mention is made of other work in this field.</div>
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