Formation of FeO2 at high pressure and its implication in Earth’s elemental cycling

来源 :第26届国际高压科学技术大会、第8届亚洲高压科技学术会议暨第19届中国高压科学技术会议(The 26th Interna | 被引量 : 0次 | 上传用户:long96169
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  The Earths iron core and the oxygen-rich atmosphere define the two end members of our planet.Charactering the distribution of Fe-O in the Earths interior and the large scale cycling of those basic elements are career pursuits of many geoscientists.
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