1) plate marginal orogenic belt
板缘造山带
1.
It is stressed that the intraplate orogenic belt is a distinct new type of orogen rather than a successor of an interplate or plate marginal orogenic belt.
指出板内造山带是一种特殊类型的造山带，而不是板缘造山带或板间造山带持续发展的结果。
2) peripheral orogen
边缘造山带
1.
This orogen saw a very complicated history from interior orogen to peripheral orogen and to interior orogen again.
该造山带经历了边缘造山带-内部造山带-边缘造山带相继转化的过程,它控制了加里曼丹的区域成矿作用,特别是晚渐新世-中中新世北加里曼丹内部造山带的逆冲叠瓦阶段是加里曼丹区域成矿的最重要时期。
3) The orogenic belts at the margin of the South China block
周缘造山带
5) intraplate orogenic belt
板内造山带
1.
The main characteristic of intraplate orogenic belts is its re mobilization of the stable lithosphere consolidated in the earlier stage There are two fundamental features of intraplate orogenic belts, i.
板内造山带的基本特征是前期已经固结的岩石圈重新活化。
2.
The different opinions concerning the concept of intraplate orogenic belt are firstly reviewed in this paper.
讨论了关于板内造山带含义的不同认识。
3.
The northern Qilian orogenic belt is an intraplate orogenic belt formed on the basis of the Neoproterozoic craton.
北祁连山是发育在新元古代大陆克拉通背景上的板内造山带，它的形成经历了三个构造发展阶段：（１） 早古生代是克拉通裂解的拗拉槽而不是大洋盆地，其西延部受阿尔金断裂左行错移约３５０ ～４００ ｋｍ ，对应于塔里木盆地北部的满加尔 阿瓦提坳陷，它们共同构成了“西域板块”之上的震旦纪 早古生代统一的拗拉槽，早古生代末“祁连事件”使拗拉槽闭合形成古祁连山。
6) continental-margin orogenic belt
大陆边缘造山带
1.
According to the tectono-geomorphological features and characteristics of neotectonic movement on the southwestern margin of the North American continent,the author has established a 3D tectonomechanic model of the reversed S-shaped continental-margin orogenic belt of the northern hemisphere.
文中根据北美大陆西南边缘造山带的构造地貌及新构造运动特征,建立了反S状大陆边缘造山带的三维构造力学模式,指出阿拉斯加地区为弧形右旋剪切隆升造山带;科迪勒拉造山带为直线右旋走滑造山带;马德雷山以南,延至加勒比海为一左旋沉降‘旋扭沟-弧-盆系统’。
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