subject predicate object context
51394 Creator 1c5c32b11b5ad1bd9c846a77784abc38
51394 Creator 96fdb8f74aad60e762b1aef18d80ab45
51394 Creator b75227dc49245aab76a534b836099ab7
51394 Creator df3dbfda1cf5802e59649f5b505eaec5
51394 Creator f959096fc292f5182e8b214c797d2544
51394 Creator fcdb1adbeb7a0307cef3a0b73443e301
51394 Creator 72eb7170d8a19be385f16460fd117c8e
51394 Creator 84764f824834b90b789fef94138093b1
51394 Creator ext-90060a5811cec207e4e5b5ac2066fe8f
51394 Creator ext-ca4be981b663b75d8b341ed478ad81b7
51394 Date 2017
51394 Date 2017-04
51394 Is Part Of p10869379
51394 Is Part Of repository
51394 abstract The Emmaville eucrite is a relatively poorly studied basaltic achondrite with an anomalous oxygen isotope signature. In this study, we report comprehensive mineralogical, petrographic, and geochemical data from Emmaville in order to understand its petrogenesis and relationship with the basaltic eucrites. Emmaville is an unusually fine-grained, hornfelsic-textured metabasalt with pervasive impact melt veins and mineral compositions similar to those of typical basaltic eucrites. The major and trace element bulk composition of Emmaville is also typical of a basaltic eucrite. Three separated individual lithologies were also analyzed for O isotopes; a dark gray fraction (E1), a shocked lithology (E2), and a lighter gray portion (E3). Fractions E1 and E2 shared similar O isotope compositions to the bulk sample (E-B), whereas the lighter gray portion (E3) is slightly elevated in Δ<sup>17</sup>O and significantly elevated in δ<sup>18</sup>O compared to bulk. No evidence for any exogenous material is observed in the thin sections, coupled with the striking compositional similarity to typical basaltic eucrites, appears to preclude a simple impact-mixing hypothesis. The O-isotopes of Emmaville are similar to those of Bunburra Rockhole, A-881394, and EET 92023, and thus distinct from the majority of the HEDs, despite having similarities in petrology, mineral, and bulk compositions. It would, therefore, seem plausible that all four of these samples are derived from a single HED-like parent body that is isotopically distinct from that of the HEDs (Vesta) but similar in composition.
51394 authorList authors
51394 issue 4
51394 status peerReviewed
51394 uri http://data.open.ac.uk/oro/document/634891
51394 uri http://data.open.ac.uk/oro/document/634892
51394 uri http://data.open.ac.uk/oro/document/634893
51394 uri http://data.open.ac.uk/oro/document/634894
51394 uri http://data.open.ac.uk/oro/document/634895
51394 uri http://data.open.ac.uk/oro/document/634896
51394 uri http://data.open.ac.uk/oro/document/662708
51394 volume 52
51394 type AcademicArticle
51394 type Article
51394 label Barrett, T. J. ; Mittlefehldt, D. W.; Greenwood, R. C. ; Charlier, B. L. A. ; Hammond, S. ; Ross, D. K.; Anand, M. ; Franchi, I. A. ; Abernethy, F. A. J. and Grady, M. M. (2017). The mineralogy, petrology, and composition of anomalous eucrite Emmavill. Meteoritics & Planetary Science, 52(4) pp. 656–668.
51394 label Barrett, T. J. ; Mittlefehldt, D. W.; Greenwood, R. C. ; Charlier, B. L. A. ; Hammond, S. ; Ross, D. K.; Anand, M. ; Franchi, I. A. ; Abernethy, F. A. J. and Grady, M. M. (2017). The mineralogy, petrology, and composition of anomalous eucrite Emmaville. Meteoritics & Planetary Science, 52(4) pp. 656–668.
51394 label Barrett, T. J. ; Mittlefehldt, D. W.; Greenwood, R. C. ; Charlier, B. L. A. ; Hammond, S. ; Ross, D. K.; Anand, M. ; Franchi, I. A. ; Abernethy, F. A. J. and Grady, M. M. (2017). The mineralogy, petrology, and composition of anomalous eucrite Emmaville. Meteoritics & Planetary Science, 52(4) pp. 656–668.
51394 sameAs maps.12818
51394 Title The mineralogy, petrology, and composition of anomalous eucrite Emmavill
51394 Title The mineralogy, petrology, and composition of anomalous eucrite Emmaville
51394 in dataset oro