1) 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。
2) 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
3) Ailaoshan-Red River structural belt
哀牢山红河构造带
1.
The Ailaoshan-Red River structural belt also underwent early lateral slip and later normal faulting.
哀牢山红河构造带同样经历早期走滑和后期正断 ,走滑年代分别为 5 8～ 5 6Ma、2 3Ma和 13Ma ,后期正断开始于 5 。
4) Ailaoshan gold minerogenetic belts
哀牢山成矿带
5) Ailaoshan-Jingshajiang belt
哀牢山-金沙江带
6) 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。
补充资料：玉溪哀牢山自然保护区
哀牢山自然保护区位于新平县与景东、镇沅、楚雄、双柏等五县交界处。海拔2080—3165.9米。1986年，云南省人民政府明文划定保护区面积是21.99万亩。1988年，经国务院批准为国家级自然保护区。
哀牢山是云岭南延支脉，第四纪喜马拉雅造山运动期间，由于地面抬升，河流下切，高差增大，而形成今天深度切割的山地地貌。由县酒江自西北向东南斜贯直下，江西部哀牢山脉与里洒江为平行走向，山川交错，山高谷深。哀牢山主峰大底岩海拔31659米，耸立在者是乡与镇流县接壤处。次峰大雪锅山海拔刀刃米，云缠雾绕，巍峨壮观，植物分布区系复杂，古老名贵植物种类较多，在气候、地质生物等方面有较高的科研价值，是自然保护区的核心区；中外科学家合作考察研究的重要基地之一。著名的大帽耳山、小帽耳山，蟀嫔玉立、千姿百态。江边一带多冲积扇和山匠，是发展粮食和热带经济作物的理想之地。江东为云南高原南部边缘地区，多属中山中切割地貌，适宜云南松和中亚热带水果生长。
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