Role of oceanic crust in deep water cycle

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：akiheeca

【摘要】

：

The mantle transition zone(MTZ)is likely to be hydrous,but the mechanism for its hydration remains to be a topic of debate.The mobilization of aqueous fluids in Earths interior is controlled by fluid

【作者】

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Liu Xingcheng Matsukage N.Kyoko Li Yuan Takahashi Eiichi Suzuki Toshihiro Nishihara Yu Xiong Xiaolin

【机构】

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State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy 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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　　The mantle transition zone(MTZ)is likely to be hydrous,but the mechanism for its hydration remains to be a topic of debate.The mobilization of aqueous fluids in Earths interior is controlled by fluid connectivity,which is usually expressed by dihedral angle of the aqueous fluids in contact with minerals.

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Role of oceanic crust in deep water cycle

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