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Szablon:Ruzicka (2014)
Z Wiki.Meteoritica.pl
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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 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 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).'' | 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 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 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).'' | ||
| + | File:Ruzicka_2014_(fig16).jpg|'''''Fig. 16.''' Cartoon showing the possible evolution of (a) [[Szablon:!Iron IVA|IVA-type]] asteroids, (b) IIE-type asteroids, and (c) [[Szablon:!Iron IAB|IAB-type]] asteroids involving collisions affecting completely to partially molten asteroids.'' | ||
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Aktualna wersja na dzień 18:35, 29 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.
.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). |
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