Origin of Graphitic Carbon and Pentlandite in Matrix Olivines in the Allende Meteorite
Origin of Graphitic Carbon and Pentlandite in Matrix Olivines in the Allende Meteorite
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Washington, DC: American Society for the Advancement of Science
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Language
English
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Washington, DC: American Society for the Advancement of Science
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Contents
Matrix olivines in the Allende carbonaceous chondrite are believed to have formed by condensation processes in the primitive solar nebula. However, transmission electron microscope observations of numerous matrix olivines show that they contain abundant, previously unrecognized, nanometer-sized inclusions of pentlandite and poorly graphitized carbo...
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Full title
Origin of Graphitic Carbon and Pentlandite in Matrix Olivines in the Allende Meteorite
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TN_cdi_proquest_miscellaneous_743738206
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_743738206
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ISSN
0036-8075
E-ISSN
1095-9203
DOI
10.1126/science.285.5432.1380