2) 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。
3) 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。
6) mantle plume magmatisme
地幔柱岩浆活动
补充资料：峨眉紫堇
罂粟科Papaveraceae
多年生草本，高50—80（100）cm。主根不规则圆柱状。基生叶与茎生叶2—6，叶片卵圆形，三回羽状分裂。总状花序顶生，有时腋生，苞片线形，萼片阔卵形，花冠淡紫红色，距细管状，长约2cm。分布于四川峨眉山，生于海拔1600—1800m处。
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