Indosinian movement was a strong pressed folding orogenic movement in company with magma activity, which was dominated by N-S direction compression.
印支期地壳以南北向挤压作用为主 ,是一次强烈褶皱造山运动 ,并伴随有强烈的岩浆活动。
Numerical Modeling of upper Mantle Convection and Orogeny of the Tianshan Mountains;
天山上地幔对流与造山运动数值模拟
Hercynian orogeny at the north margin area of Tarim North china .
显生宙以来在中国古陆块周边发生了四次大的板块碰撞或俯冲造山运动，即塔里木华北克拉通北缘及其以北地区的海西期造山运动；昆仑祁连秦岭地区的海西印支期造山运动；西南地区印支喜山期的喜马拉雅造山运动；东部大兴安岭太行山豫西鄂西湘西一线以东中生代燕山期造山运动。
synkinematic magmatism
同造山运动的岩浆酌
Maginal orogeny was formed on this condition with same relative motion trend between lithosphere and asthenosphere.
板缘造山主要表现为岩石圈和软流圈以基本相同的运动趋势的相对运动。
Plate Tectonics and Geodynamics of Orogenesis of the Southwest Tianshan Mountains;
西南天山板块构造及造山运动动力学
The period was one of general emergence and orogeny.
这个时期是全面的上升和造山运动。
The Government s "Orogeny": On Limited Politics and Unlimited Media;
政府的“造山运动”:有限政治与无限媒介
The Neotectonics in the Karakorum and West Kunlun Mountains
喀喇昆仑山-西昆仑山地区的新构造运动
Whereas the intraplate orogeny show that an inharmonious relative motion between different spheres was happened in the same region.
板内造山主要表现为同一区域内岩石圈、流圈等不同层圈之间的不协调的相对运动。
The orogenic types were controlled by the relative motion mechanism between lithosphere and asthenosphere.
板块和软流圈之间不同的相对运动机制是形成不同类型造山作用的主要原因。
Arbuckle orogeny
阿尔布克尔造山运动
alpine age orogeny
阿尔卑斯期造山运动
aectonic pluton
非造山运动深成岩体
Neo-Alpine orogenesis
新阿尔卑斯造山运动
preorogenic craton
造山运动前稳定地块
CALEDONIAN OROGENESIS AND SYSTEM-TRANSITION IN THE XUEFENGSHAN AREA
雪峰山加里东造山运动及其体制转换
Numerical Modeling of upper Mantle Convection and Orogeny of the Tianshan Mountains;
天山上地幔对流与造山运动数值模拟
On the Characteristics and Intensity of Quaternary Tectonic Movement in the Piedmont of Altai Mt.
阿勒泰山前带第四纪构造运动的特点和强度
A NEW RECOGNITION ON SPACIO-TEMPORAL CHARACTERISTICS OF THE CALEDONIAN OROGENY HAPPENED IN SOUTH CHINA
华南地区加里东期造山运动时空分布的新认识
Stratiform Geomorphology and Himalayan Tectonic Movement on the North China Mountains;
中国华北山地的层状地貌与喜马拉雅构造运动