Geology of the Kamabuseyama serpentinite unit in the Sanbagawa belt of the Kanto Mountains and implications for fluid flow along the base of the mantle wedge from 30-20 km depths
Geology of the Kamabuseyama serpentinite unit in the Sanbagawa belt of the Kanto Mountains and implications for fluid flow along the base of the mantle wedge from 30-20 km depths
复制标题
关东山脉三波川带 Kamabuseyama 蛇纹岩单元的地质及其对 30-20 km 深度沿地幔楔底部的流体流动的影响
DOI：
--
复制
发表时间：
2018
期刊：
影响因子：
--
通讯作者：
Yui Kouketsu
中科院分区：
文献类型：
--
作者：
Mari Yokota;Simon Richard Wallis;Yui Kouketsu
