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Trace element partitioning between garnet and chondritic melt from 5 to 9 GPa: implications for the onset of the majorite transition in the martian mantle

✍ Scribed by David S Draper; Dimitris Xirouchakis; Carl B Agee


Book ID
117196684
Publisher
Elsevier Science
Year
2003
Tongue
English
Weight
588 KB
Volume
139
Category
Article
ISSN
0031-9201

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