... 中华科技史学会学刊第14 期 (2010 年7 月) - 3 - 期时，遇有地壳发生造陆运动 (Epeirogenic movement)和造山运动 (Orogenesis)时，陆块 和地表乃上升，河流坡度变陡，河流再往下切，乃重新恢复到幼年期，称为回春作用 (Rejuvenation)，另外，冰河期结束或开...
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...读 关键字： 早元古代; 逆冲构造; 造山作用; 华北克拉通[gap=683]Key words: Early Proterozoic; thrust structure; orogenesis; North China Craton...
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Laurentian orogenesis 劳伦造山运动
Andean orogenesis 安第斯山型造山作用
alpinotype orogenesis 阿尔卑斯型造山作用
germanotype orogenesis 日耳曼型造山运动
polycyclic orogenesis 多旋回造山运动 ; 复相造山运动
diapiric orogenesis 挤入造山作用
monocyclic orogenesis 单旋回造山运动 ; 单相造山运动
geosynclinal orogenesis 地槽造山作用
compressional orogenesis 压性造山作用
Granites formed at all stages of collisional orogenesis, the research of their petrogenesis can promote our understanding of the nature of the orogenic. lower crust, deep dynamic orogenic process and the interactions between crust and mantle during orogenic process.
碰撞造山带中形成的花岗岩是造山作用各个阶段的重要物质记录,其源区性质和成因机制的研究对于反演造山带下地壳物质组成、造山作用深部动力学过程及造山过程中地壳和地幔物质的相互作用等科学问题具有重要意义。
参考来源 - 秦岭造山带晚三叠世花岗岩类成因机制及深部动力学背景·2,447,543篇论文数据，部分数据来源于NoteExpress
N the formation of mountain ranges by intense upward displacement of the earth's crust, usually associated with folding, thrust faulting, and other compressional processes 造山运动
They occurred under the tectonic setting ranging from post collision uplift to late orogenesis.
产生于板块碰撞后隆起到造山晚期的构造背景。
The alkali-syenites are of mantle-crust mixing type. The genesis of the rocks is associated with the orogenesis within the plate;
本区碱性正长岩类属幔壳混源成因类型，其成因与板内造山作用有关；
The intrusion of magma affected the orogenesis and deformation and it is an important geological process and factor leading nonlinear deformation.
岩浆的侵入对造山变形有重要影响，同时也是导致区域非线性变形的重要地质过程和因素。
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