
赞
的个人主页 http://grzy.cug.edu.cn/yongfeng/zh_CN/index.htm
上一条: Influence of melt-peridotite interactions on deformation and seismic properties of the upper mantle beneath a destroyed craton: A case study of the Damapong peridotites from the North China Craton
下一条: Rheology of dry K-feldspar aggregates at high temperature and high pressure: An experimental study