17 b), a negative trend between ε 48 Ca and Δ 17 O (Fig. 17 c) and between ε 54 Cr and ε 48 Ca (Fig. 17 d). 59 , 60 , 79 – 81 ) Ryugu particles plot at the highest ε 54 Cr and Δ 17 O values of these trends.
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On the origin and evolution of the asteroid Ryugu: A comprehensive geochemical perspective.
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The sentences
79 , 80 ) The carbonaceous chondrites form a positive trend between ε 54 Cr and Δ 17 O (Fig. 17 b), a negative trend between ε 48 Ca and Δ 17 O (Fig. 17 c) and between ε 54 Cr and ε 48 Ca (Fig. 17 d). 59 , 60 , 79 – 81 ) Ryugu particles plot at the highest ε 54 Cr and Δ 17 O values of these trends.