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Szablon:Ruzicka (2014)
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Ruzicka Alex, (2014), Silicate-bearing iron meteorites and their implications for the evolution of asteroidal parent bodies, Chemie der Erde, Geochemistry, 74(1), 2014, s. 3-48. Plik doi.
.jpg) Fig. 1. Oxygen isotope compositions of silicate-bearing irons. Δ17O = δ17O–0.52 δ18O. Data sources and abbreviations: TF = terrestrial fractionation line, CCAM = carbonaceous chondrite anhydrous materials mixing line, IABs and IIICDs; IIE fractionated (IIE fr.) and IIE unfractionated (IIE unfr.); IVAs; PdZ (Puente del Zacate); ungrouped irons (Ungr.) include Guin (G); Enon (E); NWA 468 (468); Sombrerete (S); Tucson (T); Mbosi (Mb); Bocaiuva (B); NWA 176 (176). Other meteorites include H, L and LL chondrite falls and finds; winonaites; mesosiderites (meso), main group pallasites (MG pall) and Eagle Station pallasites (ES pall); pyroxene pallasites (Px pall). |
