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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

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_743738206

Origin of Graphitic Carbon and Pentlandite in Matrix Olivines in the Allende Meteorite

About this item

Full title

Origin of Graphitic Carbon and Pentlandite in Matrix Olivines in the Allende Meteorite

Author / Creator

Publisher

Washington, DC: American Society for the Advancement of Science

Journal title

Science (American Association for the Advancement of Science), 1999-08, Vol.285 (5432), p.1380-1382

Language

English

Formats

Publication information

Publisher

Washington, DC: American Society for the Advancement of Science

More information

Scope and Contents

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...

Alternative Titles

Full title

Origin of Graphitic Carbon and Pentlandite in Matrix Olivines in the Allende Meteorite

Authors, Artists and Contributors

Author / Creator

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_743738206

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_743738206

Other Identifiers

ISSN

0036-8075

E-ISSN

1095-9203

DOI

10.1126/science.285.5432.1380

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