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5. The effect of trivalent cations on hydrous α-β-γ Mg2SiO4 phase transitions

The effect of trivalent cations on hydrous α-β-γ Mg2SiO4 phase transitions

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：liongliong461

【摘 要】

：

Olivine(Mg,Fe)2SiO4 with its high pressure polymorphs(β-wadsleyite,γ-ringwoodite)are the main mineral compositions in the upper mantle and the mantle transition zone.

【作 者】

：

Jiaji Jin Feiwu Zhang 

【机 构】

：

State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Scienc

【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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　　Olivine(Mg,Fe)2SiO4 with its high pressure polymorphs(β-wadsleyite,γ-ringwoodite)are the main mineral compositions in the upper mantle and the mantle transition zone.

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