The Olton, Texas, H chondrite regolith breccia - Paired with Dimmitt

Details The Olton, Texas, H chondrite regolith breccia - Paired with Dimmitt The Olton, Texas, H chondrite regolith breccia - Paired with Dimmitt

Dec 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990metic..25..259k&link_type=abstract

Meteoritics (ISSN 0026-1114), vol. 25, Dec. 1990, p. 259-261.

Computer Science

2

Breccia, Chondrites, Meteoritic Composition, Regolith, Olivine, Petrology, Rare Gases, Solar Activity Effects

Scientific paper

The Olton ordinary chondrites (two stones found in 1948) are H group,
solar wind-bearing regolith breccias. The proximity of the recovery site
to the Dimmitt strewnfield, and the similarity in texture, composition,
noble gas contents and isotopic ratios to Dimmitt indicate that Olton is
paired with Dimmitt.

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