crust mantle interaction 壳幔相互作用
mantle-crust interaction 壳幔相互作用
interaction of crust-mantle 壳幔相互作用
The igneous complexes from Xingchang, which were formed in extention tectonics, are the products of deep magmas emplacing to shallow crust. They supply petrologic evidences of crust-mantle interaction in Late Mesozoic in SE China.
新昌火成杂岩是伸展构造体制下深源岩浆浅部侵位的产物，是中国东南沿海晚中生代壳幔作用的岩石学证据。
参考来源 - 浙江新昌晚中生代火成杂岩研究·2,447,543篇论文数据，部分数据来源于NoteExpress
The results provide new evidences that the tin deposits are product of the crust-mantle interaction and that the mantle plumes had existed in the Nanling region.
这一结果为南岭地区锡多金属矿床为壳幔相互作用的产物及区域地幔柱的存在提供了新证据。
Although the volcanic rock associations formed by the three types of crust-mantle interaction are somewhat different, their magma sources all contain crustal components.
它们形成的火山岩组合有一定的差别，但源区都含有地壳组分。
Asthenosphere uplift indicates the deep adjustment process during the interaction of plates, and also shows the adjusting process of gravitational equilibrium between upper layer of crust and mantle.
软流圈隆升是板块相互作用的深部调整过程，同时也是地壳表层—地幔进行重力均衡调整的过程。
应用推荐