Discovery of an Unmelted H-Chondrite Inclusion in an Iron Metorite

Details Discovery of an Unmelted H-Chondrite Inclusion in an Iron Metorite Discovery of an Unmelted H-Chondrite Inclusion in an Iron Metorite

Apr 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995sci...268..540c&link_type=abstract

Science, Volume 268, Issue 5210, pp. 540-542

Computer Science

12

Scientific paper

The link between H chondrites and silicate inclusions in group IIE iron meteorites has long been suspected, but direct evidence for a common parentage has remained elusive. The discovery of an unmelted chondritic inclusion in the Techado iron meteorite sheds light on the genetic relation between these two groups, providing clues on the origin of chondritic materials as inclusions in iron meteorites. It is proposed that the complex IIE iron meteorite breccias formed by collisions with several different bodies, followed by deep burial of metal and silicate fragments in the asteroidal megaregolith.

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