【摘 要】
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Phase D is proposed to be the ultimate water carrier to the deep lower mantle along cold slab subduction and its elastic properties are significant for interpreting observed seismic anomalies in subdu
【机 构】
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State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,W
【出 处】
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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
论文部分内容阅读
Phase D is proposed to be the ultimate water carrier to the deep lower mantle along cold slab subduction and its elastic properties are significant for interpreting observed seismic anomalies in subducted slabs.
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