1) Dakendaban Group
达肯大坂群
1.
Redefinition of the "Dakendaban Group" on the northern margin of the Qaidam basin;
柴达木盆地北缘“达肯大坂群”的再厘定
2.
Contact relation between the Tanjianshan Group and Dakendaban Group on northern margin of Qaidam;
柴达木北缘达肯大坂群与滩间山群的接触关系
2) Dakendaba Group
达肯大坂岩群
1.
Geological Characteristics and Tectonic Setting of the Dakendaba Group in Iqe Area,Northern Margin of Qaidam Basin;
柴北缘鱼卡地区达肯大坂岩群的地质特征与构造环境
3) Daken Daban gneiss
达肯大坂片麻岩
4) Dakendaban
艾肯达坂
1.
Establishment of Tielimuke Fm. and Its Restriction on the Orogenic Period in Dakendaban,Western Tianshan;
西天山艾肯达坂一带铁木里克组的确立及对造山时限的制约
5) Aikendaban Formation
艾肯达坂组
1.
The Aikendaban Formation is a red-colored, continental volcanic sequence,unconformably overlying on the Dahalajunshan Formation of Early Carboniferous age.
西天山二叠纪艾肯达坂组红色陆相火山岩建造不整合在下石炭统大哈拉军山组之上,未经变形和变质。
2.
The Aikendaban Formation ofred-colored, continental volcanic sequence well developed in the Aikendaban area, West Tianshan.
西天山艾肯达坂地区较好发育了艾肯达坂组红色陆相火山岩建造,它不整合在下石炭统大哈拉军山组之上,未经变形和变质,属于陆陆碰撞晚期的橄榄安粗岩系,其年龄确定是厘定从碰撞造山向陆内构造演化的关键。
6) Tokuzidaban Group Midformation
托库孜达坂群中组
补充资料:达坂
1.源于蒙语dabaya(n)。山口;山岭。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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