他发现了地幔的上边界,即我们所熟知的莫霍维奇不连续面(Mohorovičić discontinuity),或简称莫霍面(Moho)。该边界标志着地球内部主体的开始,它从地壳的底部(大陆下30-60km,大洋薄地壳近~6km)一直到2890km处的...
基于12个网页-相关网页
以上来源于: WordNet
N the boundary between the earth's crust and mantle, across which there is a sudden change in the velocity of seismic waves 莫霍界不连续界面 (Often shortened to Moho)
应用推荐