1) Ailao Shan metamorphic belt
哀牢山变质带
1.
Ailao Shan metamorphic belt can be subdivided into two metamorphic belts from their characteristics of metamorphism and deformation, a high-grade metamorphic belt in the east and a low-grade metamorphic belt in the west.
哀牢山变质带可以划分为两种不同变质变形特点的变质带:东部高级变质带和西部低级变质带,自北东向南西依次为三条边界断裂:红河断裂、哀牢山断裂和九甲—安定断裂。
2) Ailaoshan epi-metamorphic rock belt
哀牢山浅变质岩带
1.
Ailaoshan epi-metamorphic rock belt is distributed in Paleozoic and Mesozoic strata between Ailaoshan and Jiujia-Anding deep faults.
哀牢山浅变质岩带分布于哀牢山深大断裂与九甲—安定深大断裂之间的古生界与中生界地层中,哀牢山金矿带目前已发现的主要金矿床(点)均产于其中,金矿类型以蚀变岩型和石英脉型为主,但近年来,相继发现了一批红土型金矿。
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：小牢
1.少牢。
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