喜马拉雅运动 meaning in Chinese
himalaya movement
himalayan movement
himalayan orogeny
himalayanmovement
Examples
- On the influence of global change of cenozoic climate and uplift of himalayas , the area began to present a distinct seasonal climate on the basis of previous warmth and humidity in pliocene
受新生代全球气候变冷和喜马拉雅运动的影响，该盆地一方面受印度洋季风的影响增强，干湿季节交替明显；另一方面受地形地貌影响，沿袭了温暖湿润的气候条件。 - In himalayan , the first era ( 45ma ) the basin is titled ; the second era ( 23ma ) it is differential uplift and denude ; the third era it is brittle defonnation . in eastern ore belt , ore - controlling is mainly strike - slip fault and fold ; but in western ore belt , it is block
喜马拉雅运动第一期45ma盆地掀斜；第二期23ma以差异隆升剥蚀为主；第三期4ma为脆性变形期，东矿带近盆边以走向断裂及褶皱控矿为主，西矿带为断块控矿。 - The dislocation interfaces , which have different directions , different combinations , different scale , different deformation strength and different properties , are belonged to shallow structure . they are the products of multi - stages , multi - periods and multi - causes of movement during the himalayan epoch . they were controlled by and resulted from 2 structural stress fields of ne structure and nw structure
由此认识到，坝区发育的不同方向、不同形态和组合型式、不同规模、不同变形强度和不同性质的错动带属于地壳浅部构造层次，是本区喜马拉雅运动多期次、多阶段、多成因的构造产物，分属于区域上ne向构造带和nw向构造带的构造成分，并受控于这两期构造的构造应力场。 - 2 . 38 . 6ma and 36 . 7ma isotopic ages of quartz - monzonite - porphyry in lianhuashan and alkaline porphyry in zhuopan have respectively been obtained . those results are consistent with the ages of the porphyries in both lanping - shimao basin and changdu basin related igneous rocks , representing the first episode ( lanping movement ) of tectonics - magmatism - metallogenic event during the himalayan movement
获得了莲花山石英二长斑岩及卓潘碱性斑岩的ar - ar年龄，分别为38 . 6ma与36 . 7ma ，与整个兰坪?思茅盆地与昌都盆地及两侧的斑岩与相关火山岩一致，代表喜马拉雅运动第一幕(兰坪运动)的重要构造?岩浆?成矿事件。 - Based on the structural evolution and geological framework in northern margin rift of qaidam basin , this paper presents that the overall course of faults development in middle qaidam is the main power for controlling the superimposition and assemblage of mesozoic and cenozoic basins , the deep sedimentary structure of mesozoic and the reverse structures during himalayan movement in this rift , and illustrates that the petroleum system in it is characterized by side - by - side pattern in space and by continuous pattern in time
摘要在分析研究柴北缘断陷构造演化和地质结构的基础上，指出柴中断层发育的全过程，是控制柴北缘断陷中、新生界盆地的叠加与组合、中生界深层沉积构造和喜马拉雅运动期构造反转等形成的主要动力，进而阐明?柴北缘断陷含油气系统在空间上为并列型、在时间上为连续型的特徵。