Ailaoshan

基本解釋

It is a backland basin of Ailaoshan orogenic belt instead of a foreland basin as some geologists have considered.
它與哀牢山造山帶西側(cè)的前陸盆地雖然同時(shí)發(fā)生，但其形成的沉積環(huán)境和巖石組合并不相同。
These alklic rocks are mainly distributed over the east side of Ailaoshan Deep Fault. Mid-Yunnan Basin is only a part of the distributing area.
此類堿性巖主要分布于哀牢山斷裂東側(cè),滇中盆地僅是其分布地區(qū)的一個(gè)部分。
According to preliminary investigations, Ailaoshan Nature Reserve, Chuxiong, a total area of two double 86 kinds of mammals, 27 families belong, is 63.
據(jù)初步調(diào)查，哀牢山自然保護(hù)區(qū)楚雄、雙柏兩個(gè)分區(qū)共有哺乳動(dòng)物86種，分隸27科、63屬。
Ailaoshan obviously stands between the two peteridophyte diversity centers of China, northwest Yunnan and southeast Yunnan, functioning as the linkage.
哀牢山明顯處于滇西北、滇東南這兩大中國(guó)特有多樣性中心之間，成為聯(lián)系的紐帶。
The Jinping fault block is one of the most advantageous metallogenetic belt in southeast of the Ailaoshan metallogenetic belt.
金平斷塊是哀牢山成礦域東南地區(qū)最有利的成礦帶,成礦與斷裂帶關(guān)系密切,礦帶的展布亦嚴(yán)格受構(gòu)造控制。