1) Emei mantle plume
峨眉地幔热柱
1.
Chinese carlin-type gold deposits are mainly located in the "Yunnan -Guizhou -Guangxi", "Sichuan-Gansu-Shanxi" and the west of Yunnan region, which are located in the area of Emei mantle plume activity.
“滇黔桂”、“川甘陕”及“滇西”地区均位于峨眉地幔热柱活动区。
2) Emei mantle plume
峨眉地幔柱
1.
New advances in geochronologic study related to Emei mantle plume and their significance;
与峨眉地幔柱有关年代学研究的新进展及其意义
2.
The picrite field, located in the southwest of Emeishan continental flood basalts (ECFB) and with the center in Lijiang—Dali—Panzhihua triangular area, is about 5×104 km2 and regarded as the axial area of the Emei mantle plume.
峨眉山大陆溢流玄武岩(ECFB)的西南部以丽江、大理和攀枝花三角区为中心的苦橄岩分布区,面积约5×10 4 km2 ,为峨眉地幔柱的轴部区。
4) Emeishan mantle plume
峨眉山地幔柱
1.
The paper gives a brief description of the metallogenic types and distinguishing features of mineralization connected with the Emeishan mantle plume.
概述了峨眉山地幔柱成矿作用的基本类型和主要特点,对主要成矿类型包括地幔柱活动直接形成的岩浆矿床和地壳响应形成的间接矿床作了全面的分析介绍,初步勾画了峨眉山大火成岩省地幔柱成矿作用的基本框架。
5) 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。
6) Plume
[英][plu:m] [美][plum]
热地幔柱
补充资料：峨眉无柱兰
兰科Orchidaceae
多年生陆生兰，高6-12cm。叶线状披针形。花1-2，顶生，粉红色，唇瓣伸展，3裂，中裂片2浅裂，距显著。分布于湖南、湖北、陕西、甘肃、四川、云南、广西、贵州。
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参考词条