Silicate diffusion in alkali-carbonatite and hydrous melts at 16.5 and 24 GPa : Implication for the melt transport by dissolution-precipitation in the transition zone and uppermost lower mantle
Silicate diffusion in alkali-carbonatite and hydrous melts at 16.5 and 24 GPa : Implication for the melt transport by dissolution-precipitation in the transition zone and uppermost lower mantle
复制标题
16.5 和 24 GPa 下碱碳酸盐岩和含水熔体中的硅酸盐扩散:对过渡带和最上部下地幔中溶解-沉淀的熔体输运的影响
DOI:
10.1016/j.pepi.2013.09.004
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发表时间:
2013
期刊:
影响因子:
--
通讯作者:
et al.
中科院分区:
文献类型:
--
作者:
A. Shatskiy;et al.