1) marginal active belt
边缘活动带
2) active margin
活动边缘
1.
In the Triassic, the sedimentary structural zones developed from passive margin basin to active margin basin as a result of the influence of the Jinshajiang suture zone and Garz Litang suture zone,and split apart into the Baiyu Yidun foreland basin,Chomta Xiangcheng island arc zone and Yulong Daocheng fore.
在三叠纪时期受金沙江缝合带与甘孜—理塘缝合带构造作用的相互影响，其沉积构造性质也由被动边缘盆地演化为活动边缘盆地，同时分裂为白玉—义敦前陆盆地，昌台—乡城岛弧带、玉隆—稻城弧前盆地。
2.
Present situation of genesis of retroarc basin and its sequence stratigraphy is outlined On the basis of case studies at home and abroad,sequence stratigraphical features in setting of active margin are discussed Study of outcrop sequence stratigraphy in setting of retroarc basin is workabl
在简述弧后盆地成因及其层序地层研究现状之后，通过国内外比较典型例子的对比分析，探讨活动边缘层序地层特征，并认为在弧后盆地开展露头层序地层工作是可行的。
3) epicontinental mobile belt faulted sag trough
大陆边缘活动带裂陷槽
4) Edge active measure
边缘活动度
5) activity of edge layer
边缘层活动
6) active continential margin
活动陆缘带
补充资料：板带轧制速度规程(见板带轧制规程设计)
板带轧制速度规程(见板带轧制规程设计)
speed schedule for plate and strip rolling
bandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
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