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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{{!Page-number|page={{{page|}}}}}. Plik {{!doi|10.1016/j.chemer.2013.10.001}}.<noinclude>
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{{!Page-number|page={{{page|}}}}}. Plik {{!doi|10.1016/j.chemer.2013.10.001}}.<noinclude>
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File:Ruzicka_2014_(fig01).jpg|'''''Fig. 1.''' Oxygen isotope compositions of silicate-bearing irons. Δ<sup>17</sup>O = δ<sup>17</sup>O–0.52&nbsp;δ<sup>18</sup>O. Data sources and abbreviations: TF = terrestrial fractionation line, CCAM = carbonaceous chondrite anhydrous materials mixing line, IABs and IIICDs; IIE fractionated (IIE&nbsp;fr.) and IIE unfractionated (IIE&nbsp;unfr.); IVAs; PdZ (Puente del Zacate); ungrouped irons (Ungr.) include Guin (G); Enon (E); NWA&nbsp;468 (468); Sombrerete (S); Tucson (T); Mbosi (Mb); Bocaiuva (B); NWA&nbsp;176 (176). Other meteorites include H, L and LL chondrite falls and finds; winonaites; mesosiderites (meso), main group pallasites (MG&nbsp;pall) and Eagle Station pallasites (ES&nbsp;pall); pyroxene pallasites (Px&nbsp;pall).''
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Aktualna wersja na dzień 09:49, 27 cze 2025

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.



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