Minor Element Zoning of Olivine in Type IIA Chondrules in Semarkona

Details Minor Element Zoning of Olivine in Type IIA Chondrules in Semarkona Minor Element Zoning of Olivine in Type IIA Chondrules in Semarkona

Mar 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009lpi....40.1669h&link_type=abstract

40th Lunar and Planetary Science Conference, (Lunar and Planetary Science XL), held March 23-27, 2009 in The Woodlands, Texas, i

Physics

1

Scientific paper

P-rich zones, preserved because P diffuses slowly, mark periods of rapid
growth and generally show continuous crystallization of olivine grains.
They also mark onset of growth on resorbed relict grains. P X-ray maps
can clarify the evolution of individual chondrules.

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