1) congregating and exhaling of mantle heat energy
地幔热能聚散
2) mantle plume
地幔热柱
1.
The ore-forming materials are mainly derived from the earth core constrained by deep processes and moved up to surface with multi-stages of mantle plume evolution and is contaminated with earth crust materials.
认为峪耳崖矿区成矿物质应主要来自地核,受深部过程的约束,成矿物质随地幔热柱多级演化向地表迁移,在其上升过程中,与壳源物质发生部分混染,使所测同位素数据往往表现出以深源为主、并混有少量壳源物质的特征。
2.
Mantle branch is the third-grade tectonic unit during multiple evolution of mantle plume.
幔枝构造是地幔热柱多级演化的三级单元,其对内生矿产的成矿控矿作用十分明显。
3.
Mantle branch structure is the third-order unit of mantle plume multistage evolution.
幔枝构造是地幔热柱多级演化的第三级构造单元 ,其核部变质—岩浆杂岩隆起与外围盖层之间的主拆离带体系是很好的成矿控矿构造。
3) Mantle hotspot
地幔热点
4) mantle heat flow
地幔热流
5) Plume
[英][plu:m] [美][plum]
热地幔柱
6) Sub-mantle plume
地幔亚热柱
1.
According to the study of mantle plume for ten years,it is concluded that sub-mantle plume is strongly uplifting under fault basin of North China.
笔者依据近十余年华北地幔亚热柱的研究认为 ,华北断陷区之下为一强烈上隆的地幔亚热柱。
补充资料：聚散障
聚散障
聚散障 病证名。见路际平《眼科临症笔记》，也即聚开障。详见该条。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条