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1)  Yidun island arc belt
义敦岛弧带
2)  Yidun island arc
义敦岛弧
1.
Evolution of Triassic volcanic-sedimentary basins in the central segment of the Yidun island arc of the Songpan-Garzê orogenic belt,western Sichuan,China;
松潘-甘孜造山带义敦岛弧中段三叠纪火山-沉积盆地的演化
2.
Age of intraplate volcanism in the back-arc area of Yidun island arc and its significance;
义敦岛弧带弧后区板内岩浆作用的时代及意义
3.
Zhujiding porphyry copper deposit is located in the north part of the "Three-river" metallogenic belt,and in the south part of non-ferrous and precious metal concentration region of Yidun island arc.
竹鸡顶铜矿位于著名的多金属成矿带西南三江成矿带北带,义敦岛弧有色、贵金属矿产地集中区南部。
3)  Yidun arc
义敦岛弧
1.
The Nongduke deposit is the first volcanic epithermal Au_Ag polymetallic deposit found in the Yidun arc zone.
农都柯矿床是在义敦岛弧带中首次发现的火山岩型浅成低温Au_Ag多金属矿床。
2.
As a composite orogenic belt of the Himalaya giant orogenic zone, Yidun arc, Sanjiang region (means three rivers region, i.
三江义敦岛弧是喜马拉雅巨型造山带中的一个复合造山带,它具有复杂的构造演化历史、代表性的岩浆活动、典型的矿床分布及相应的成矿作用。
4)  North end of the Yidun island arc
义敦岛弧北端
5)  island arc belt
岛弧带
1.
Since the middle and late Caledonian, the two basins beg3n opening and closins,and three subduction zones, two collision zones andseven island arc belts were formed.
从加里东中晚期开始,两个洋盆边拉张达消减,形成3条俯冲带、2个对接带和7个岛弧带,最后于华力西中期沿克拉表里、康古尔塔格两个对接带闭合。
6)  Yidun metallogenic belt
义敦成矿带
1.
Lying in a special geotectonic position and undergoing complicated geological evolution and strong magmatism, Yidun metallogenic belt is rich in mineral resources.
义敦成矿带地处独特的大地构造部位 ,经历了复杂的地质构造演化和强烈的岩浆活动 ,成矿条件优越 ,矿产资源丰富。
补充资料:可敦
1.见"可贺敦"。
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