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5. Revealing Iron Isotopic Fractionation in Earth’s Lower Mantle and Core by Inelastic X-ray Scattering

Revealing Iron Isotopic Fractionation in Earth’s Lower Mantle and Core by Inelastic X-ray Scattering

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：xsnxj111

【摘 要】

：

Iron is by far the most abundant transition metal in the solar system and in the Earths interior.Its extreme abundance and unique electronic states have shaped the evolution of the planet.

【作 者】

：

Jung-Fu Lin 

【机 构】

：

Center for High Pressure Science and Technology Advance Research,Shanghai,201203,China;Department of

【出 处】

：

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

【发表日期】

：

2017年10期

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　　Iron is by far the most abundant transition metal in the solar system and in the Earths interior.Its extreme abundance and unique electronic states have shaped the evolution of the planet.

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