1) intraplate orogeny
板内造山
1.
Late Cenozoic intraplate orogeny and dynamic metallogeny in the southern Qinghai-Tibet Plateau;
青藏高原南部晚新生代板内造山与动力成矿
2.
Characters of Later Jurassic Yinshan Intraplate Orogeny Belt——Evidence from Daqing Shan,Inner Mongolia
阴山晚中生代板内造山特征及其动力机制——以内蒙古大青山为例
3.
Involved in the Cenozoic intraplate orogeny of southwestern Tianshan,the northwestern Tarim Basin had developed a series of NE-trending faults and fault-related folds.
塔里木盆地西北部卷入了西南天山新生代板内造山活动,以发育一系列北东向展布的断层和断层相关褶皱为特征,但该区新生代构造变形的原因尚存在争议。
2) 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。
3) Yanshan Intraplate orogen
燕山板内造山带
1.
On Yanshan intraplate orogene: An example from Taiyanggouarea, Lingyuan, western Liaoning Province, Northeast China;
燕山板内造山带早期构造变形演化——以辽西凌源太阳沟地区为例
5) Intraplate orogenesis
板内造山作用
6) intraplate orogeny
板内造山作用
1.
The Mesozoic intraplate orogeny of the Taihang Mountains and the thinning of the continental lithosphere in North China;
太行山中生代板内造山作用与华北大陆岩石圈巨大减薄
2.
On the basic features of the regional geological tectonics of China—The key to understanding of the Cenozoic intraplate orogeny;
新生代板内造山作用研究——认识中国区域地质构造基本特征的关键
补充资料：内造人儿
1.犹家生子儿。指奴仆的子女仍在主人家当差的。
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