TRACING PLANETARY DIFFERENTIATION PRESSURE AND OXYGEN FUGACITY CONDITIONS USING NI AND CO METAL/SILICATE PARTITIONING: APPLICATION TO THE ACHONDRITE PARENT BODIES

被引:0
|
作者
Cartier, C. [1 ]
Llado, L. [1 ,2 ]
Pirotte, H. [2 ]
Tissandier, L. [1 ]
Namur, O. [3 ]
Collinet, M. [4 ]
Wang, S. -J. [5 ]
Charlier, B. [2 ]
机构
[1] Univ Lorraine, CNRS, CRPG, Nancy, France
[2] Univ Liege, Dept Geol, Sart Tilman Par Liege, Belgium
[3] Katholieke Univ Leuven, Dept Earth & Environm Sci, Heverlee, Belgium
[4] UNamur, Dept Geol, Namur, Belgium
[5] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing, Peoples R China
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中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
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页码:A56 / A56
页数:1
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