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Forsteritic Olivine Grains in Unequilibrated Ordinary Chondrites: Additional Evidence for a Link Between Ordinary and Carbonaceous ChondritesWe report mineral-chemical and Secondary Ion Mass Spectrometry (SIMS) oxygen-isotopic studies of forsteritic olivine grains from various Unequilibrated Ordinary Chondrites (UOCs). Our studies provide additional evidence for a genetic link between ordinary and carbonaceous chondrites and between various lithologies in these meteorites.
Document ID
20000081227
Acquisition Source
Headquarters
Document Type
Conference Paper
Authors
Ruzicka, A. (Portland State Univ. OR United States)
Hiyagon, H. (Tokyo Univ. Japan)
Prinz, M. (American Museum of Natural History New York, NY United States)
Taylor, L. A. (Tennessee Univ. Knoxville, TN United States)
Date Acquired
August 19, 2013
Publication Date
March 1, 2000
Publication Information
Publication: Lunar and Planetary Science XXXI
Subject Category
Lunar And Planetary Science And Exploration
Funding Number(s)
CONTRACT_GRANT: NAGW-3543
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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