In-situ X-ray diffraction and Raman spectroscopic studies on CaFe2O4-type β-CaCr2O4 under high press

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:danble
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  The CaFe2O4-type structure was believed as the high-pressure form of many spinels at the pressure and temperature conditions corresponding to the mantle transition zone and upper border of the lower mantle of the Earth [1,2,3].
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