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The Olton, Texas, H chondrite regolith breccia - Paired with DimmittThe 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.
Document ID
19910041005
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Keil, Klaus
(University of Hawaii at Manoa Honolulu, United States)
Ehlmann, A. J.
(Texas Christian University Fort Worth, TX, United States)
Wieler, Rainer
(Zuerich Eidgenoessische Technische Hochschule, Zurich, Switzerland)
Date Acquired
August 14, 2013
Publication Date
December 1, 1990
Publication Information
Publication: Meteoritics
Volume: 25
ISSN: 0026-1114
Subject Category
Lunar And Planetary Exploration
Accession Number
91A25628
Funding Number(s)
CONTRACT_GRANT: NAG9-454
Distribution Limits
Public
Copyright
Other

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