subject predicate object context
32386 Creator 1c5c32b11b5ad1bd9c846a77784abc38
32386 Creator b75227dc49245aab76a534b836099ab7
32386 Creator 84764f824834b90b789fef94138093b1
32386 Creator a5c0a605ec7472b7ee96eb656061979e
32386 Creator ext-a308bec7ea7a58b2ecdd7c3eedf317a4
32386 Date 2011
32386 Is Part Of repository
32386 abstract Introduction: Silicate inclusions have been observed in about half of all currently identified IIE irons (21 specimens). Based mainly on their similar oxygen isotope compositions, a genetic relationship between the IIE irons and H chondrites had been proposed. However, this relationship was subsequently questioned due to the limited overlap between laser fluorination data for equilibrated H chondrites and the earlier IIE silicate data. We are undertaking a detailed oxygen isotope and geochemical study of both the IIE silicate inclusions and H chondrites, with the aim of investigating further the relationship between the two groups.
32386 authorList authors
32386 presentedAt ext-b70af2161a5f6ee32b2ad1b451469793
32386 status peerReviewed
32386 type AcademicArticle
32386 type Article
32386 label McDermott, K. H. ; Greenwood, R. C. ; Franchi, I. A. ; Anand, M. and Scott, E. R. D. (2011). The relationship between IIE irons and H chondrites: petrologic and oxygen isotope constraints. In: 74th Annual Meeting of the Meteoritical Society, 8-12 Aug 2011, London, UK.
32386 label McDermott, K. H. ; Greenwood, R. C. ; Franchi, I. A. ; Anand, M. and Scott, E. R. D. (2011). The relationship between IIE irons and H chondrites: petrologic and oxygen isotope constraints. In: 74th Annual Meeting of the Meteoritical Society, 8-12 Aug 2011, London, UK.
32386 Title The relationship between IIE irons and H chondrites: petrologic and oxygen isotope constraints
32386 in dataset oro