Nickel Abundance of Olivine and Magnetite in CV and CK Chondrites: Evidence for a Continuous Metamorphic Sequence?

Details Nickel Abundance of Olivine and Magnetite in CV and CK Chondrites: Evidence for a Continuous Metamorphic Sequence? Nickel Abundance of Olivine and Magnetite in CV and CK Chondrites: Evidence for a Continuous Metamorphic Sequence?

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2043d&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2043

Physics

Scientific paper

We examine the suggestion that the CK and CV chondrites were derived
from a single, thermally stratified asteroid by using NiO content in
magnetite to look for a continuous metamorphic sequence between the two
groups.

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