1) Ailao Mountain belt
哀牢山带
1.
Late Devonian (D 3) silicate and Early Carboniferous (C 1) silicate in Ailao Mountain belt, “Three_River” area, are quite different from each other in mode of occurence, Radiolaria association, Si isotope and REE character.
“三江”地区哀牢山带晚泥盆世和早石炭世硅质岩的产状、放射虫组合、硅同位素及稀土元素特征有明显的差异 :前者属于深海环境 ,当时为陆内裂谷 ;后者属于哀牢山蛇绿岩套组成单元 ,形成于半深海环境 ,表明当时哀牢山是一个小洋
2) Ailaoshan orogenic belt
哀牢山造山带
1.
Based on the recently known data of is otopic dating and tectonolithostra tigraphic units of the Ailaoshan area,tectonic evolution s of the Ailaoshan orogenic belt have been reconsidered.
依据新获得的同位素年代学资料和构造岩石地层单元,重新认识了云南哀牢山造山带形成与演化历史。
3) Ailaoshan gold minerogenetic belts
哀牢山成矿带
4) Ailaoshan-Jingshajiang belt
哀牢山-金沙江带
5) Ailaoshan gold mineralization belt
哀牢山金矿带
1.
The study of composition and physico-chemical characteristics of fluid inclusions from three gold deposits hosted in the Ailaoshan gold mineralization belt indicated that the ore-forming fluid was characterized as being rich in Na+, K+, Cl-,SO2-4,F-and CO2, and belongs to the Na type solution, epi- to mesothermal in nature, moderately saline, intermediate to weak alkaline, and relatively reducing.
本文系统研究了哀牢山金矿带主要金矿床主成矿阶段石英流体包裹体的化学组成和物理化学性质。
6) Ailaoshan fault belt
哀牢山断裂带
1.
Lamprophyres in the Baimazhai nickel deposit are located on the southern segment of Ailaoshan fault belt.
白马寨镍矿区煌斑岩位于哀牢山断裂带的南段,是该条带上新生代富钾火成岩的重要组成部分。
补充资料：上牢
1.谓牛羊豕等美味。牢，古代祭祀用的牺牲。
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