Evidence for the Presence of Alkalis at High Temperatures in Type II Chondrules in Ordinary Chondrites

Details Evidence for the Presence of Alkalis at High Temperatures in Type II Chondrules in Ordinary Chondrites Evidence for the Presence of Alkalis at High Temperatures in Type II Chondrules in Ordinary Chondrites

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.2084g&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

1

Scientific paper

Type II chondrules in Semarkona formed as relatively simple igneous
systems. Na contents varied, but were generally high during the entire
cooling history. However, the chondrules were likely open to Na loss or
gain at low temperatures.

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