Mineral association of sulfide nodules of the Burkhala iron meteorite and the conditions of its formation

Details Mineral association of sulfide nodules of the Burkhala iron meteorite and the conditions of its formation Mineral association of sulfide nodules of the Burkhala iron meteorite and the conditions of its formation

Jun 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989geokh......825i&link_type=abstract

Geokhimiia (ISSN 0016-7525), June 1989, p. 825-837. In Russian.

Computer Science

Iron Meteorites, Meteoritic Composition, Nodules, Sulfides, Olivine, Phase Diagrams, Pyroxenes, Troilite, Zinc Sulfides

Scientific paper

Data are presented on the chemical compositions of the troilite, dobreelite, alabandine, zinc sulfides, olivine, pyroxene, and manganochromite from the Burkhala meteorite, showing an absence of equilibrium in the component association. These data do not support the possibility of formation of the Burkhala minerals inside a large parental meteorite body. A hypothesis is proposed according to which sulfides in the Burkhala meteorite formed under the condition of secondary reductions of precursory mineral phases, followed by their melting and rapid solidification.

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