1) 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。
2) Ailao Shan-Red River fault zone
哀牢山3/红河断裂带
3) 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
4) 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。
5) Ailaoshan gold minerogenetic belts
哀牢山成矿带
6) Ailaoshan-Jingshajiang belt
哀牢山-金沙江带
补充资料：下牢
1.即下牢关，在今湖北宜昌市西北。
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