Matches in SemOpenAlex for { <https://semopenalex.org/work/W4288941197> ?p ?o ?g. }
- W4288941197 endingPage "1758" @default.
- W4288941197 startingPage "1745" @default.
- W4288941197 abstract "Abstract Isotopic compositions of O, Mo, and Cu in the IIE iron meteorites have indicated a close affinity to the H chondrite group. The diversity of trace element compositions and their abundance of silicate inclusions indicate that IIE iron meteorites were formed in multistage processes. To better constrain the formation of the IIE irons, this study analyzed elemental abundances in the metal of five IIE irons (Elga, Miles, Tobychan, Verkhne Dnieprovsk, and Watson) by laser ablation inductively coupled plasma mass spectrometry. The data are interpreted in terms of a new model of IIE crystallization from the metal fraction of completely molten H chondrite‐like material based on the solid/liquid distribution coefficients of siderophile and chalcophile elements changing simultaneously with changes of S concentrations in the remaining liquid during the crystallization of the Fe,Ni phase in the Fe‐Ni‐S system. The model showed that IIE iron compositions could be produced as solid phases at 40–73 wt% of fractional crystallization of the metal component of a bulk H chondrite‐like metallic melt. We propose that IIE iron metal could have originated from the solidified core of a differentiated body of H chondrite‐like composition and sampled different fractions of that core exposed during a catastrophic disruption of the body. The present structure of metal and silicate inclusions of IIE irons was formed by remelting and metal–silicate mixing during late impact event(s) on the parent body surface." @default.
- W4288941197 created "2022-07-31" @default.
- W4288941197 creator A5010638543 @default.
- W4288941197 creator A5015877364 @default.
- W4288941197 creator A5049172834 @default.
- W4288941197 creator A5085877860 @default.
- W4288941197 date "2022-07-31" @default.
- W4288941197 modified "2023-09-27" @default.
- W4288941197 title "Geochemical evidence for the origin of the IIE parent body from H chondrite‐like material" @default.
- W4288941197 cites W1535385535 @default.
- W4288941197 cites W1846057075 @default.
- W4288941197 cites W1963634388 @default.
- W4288941197 cites W1970430961 @default.
- W4288941197 cites W1976875638 @default.
- W4288941197 cites W1977457396 @default.
- W4288941197 cites W1980325965 @default.
- W4288941197 cites W1983413384 @default.
- W4288941197 cites W1983485353 @default.
- W4288941197 cites W1988732794 @default.
- W4288941197 cites W1990196706 @default.
- W4288941197 cites W2005319343 @default.
- W4288941197 cites W2007377514 @default.
- W4288941197 cites W2008607114 @default.
- W4288941197 cites W2010659865 @default.
- W4288941197 cites W2012034224 @default.
- W4288941197 cites W2014604070 @default.
- W4288941197 cites W2016611062 @default.
- W4288941197 cites W2024349421 @default.
- W4288941197 cites W2028874730 @default.
- W4288941197 cites W2045566045 @default.
- W4288941197 cites W2050496780 @default.
- W4288941197 cites W2051047092 @default.
- W4288941197 cites W2051410728 @default.
- W4288941197 cites W2052048955 @default.
- W4288941197 cites W2052546748 @default.
- W4288941197 cites W2053196564 @default.
- W4288941197 cites W2054982398 @default.
- W4288941197 cites W2056511558 @default.
- W4288941197 cites W2057820877 @default.
- W4288941197 cites W2059163403 @default.
- W4288941197 cites W2060260265 @default.
- W4288941197 cites W2060462572 @default.
- W4288941197 cites W2063265655 @default.
- W4288941197 cites W2070542211 @default.
- W4288941197 cites W2073100644 @default.
- W4288941197 cites W2074094597 @default.
- W4288941197 cites W2076585944 @default.
- W4288941197 cites W2079507389 @default.
- W4288941197 cites W2089901019 @default.
- W4288941197 cites W2094580905 @default.
- W4288941197 cites W2096607453 @default.
- W4288941197 cites W2100451940 @default.
- W4288941197 cites W2101453293 @default.
- W4288941197 cites W2108670073 @default.
- W4288941197 cites W2115065562 @default.
- W4288941197 cites W2148947880 @default.
- W4288941197 cites W2151276943 @default.
- W4288941197 cites W2166406131 @default.
- W4288941197 cites W2169812777 @default.
- W4288941197 cites W2541184075 @default.
- W4288941197 cites W2547970397 @default.
- W4288941197 cites W2605447251 @default.
- W4288941197 cites W2768634266 @default.
- W4288941197 cites W2791000125 @default.
- W4288941197 cites W2899933192 @default.
- W4288941197 cites W2937927568 @default.
- W4288941197 cites W2964846605 @default.
- W4288941197 cites W2965874334 @default.
- W4288941197 cites W2966569799 @default.
- W4288941197 cites W2978399941 @default.
- W4288941197 cites W3131169166 @default.
- W4288941197 cites W3185239680 @default.
- W4288941197 doi "https://doi.org/10.1111/maps.13898" @default.
- W4288941197 hasPublicationYear "2022" @default.
- W4288941197 type Work @default.
- W4288941197 citedByCount "0" @default.
- W4288941197 crossrefType "journal-article" @default.
- W4288941197 hasAuthorship W4288941197A5010638543 @default.
- W4288941197 hasAuthorship W4288941197A5015877364 @default.
- W4288941197 hasAuthorship W4288941197A5049172834 @default.
- W4288941197 hasAuthorship W4288941197A5085877860 @default.
- W4288941197 hasConcept C116862484 @default.
- W4288941197 hasConcept C11872896 @default.
- W4288941197 hasConcept C121332964 @default.
- W4288941197 hasConcept C127313418 @default.
- W4288941197 hasConcept C130635790 @default.
- W4288941197 hasConcept C17409809 @default.
- W4288941197 hasConcept C178790620 @default.
- W4288941197 hasConcept C185592680 @default.
- W4288941197 hasConcept C191897082 @default.
- W4288941197 hasConcept C192562407 @default.
- W4288941197 hasConcept C199289684 @default.
- W4288941197 hasConcept C203036418 @default.
- W4288941197 hasConcept C2777108582 @default.
- W4288941197 hasConcept C2777335606 @default.
- W4288941197 hasConcept C2778994143 @default.
- W4288941197 hasConcept C2779517257 @default.
- W4288941197 hasConcept C2780609349 @default.