喜马拉雅运动

喜马拉雅运动的影响使本区构造复杂化。形成NE向扭性断层；

The structures that are influenced by Himalayan movement take on complexity .

运用有限元法的SSFM应力场模拟软件，对准噶尔盆地南缘喜马拉雅运动期构造应力场进行了模拟。

By using SSFM simulator of finite element method , this paper presents the simulation of tectonic stress field in the southern margin of Junggar basin during Himalayan movement .

喜马拉雅运动使川东北地区遭受抬升剥蚀，储集层温度降至低于120℃，TSR反应停止。

The Himalayan orogeny caused the uplift and erosion of NE Sichuan area , the reservoir temperature fell to less than 120 ℃ and the TSR ended .

喜马拉雅运动第一期45Ma盆地掀斜；

In Himalayan , the first era ( 45Ma ) the basin is titled ;

喜马拉雅运动使本区发育为类前陆盆地。

Himalayan movement made the area developed as a para-foreland basin .

圈闭主要形成于喜马拉雅运动期。

Traps here were mostly formed in the Himalayan movement period .

库车前陆盆地喜马拉雅运动特征及其油气地质意义

Characteristics and petroleum geological significance of Himalayan orogeny in Kuqa foreland basin

中国喜马拉雅运动的期次及其动力学背景

Episodes and geodynamic setting of Himalayan movement in China

喜马拉雅运动与准噶尔盆地南缘油气成藏

Relationship between Himalayan Movement and Hydrocarbon Accumulation in Southern Margin of Junggar Basin

喜马拉雅运动对库车坳陷油气成藏的影响

Influence of Himalayan Orogeny on Oil Gas Forming in Kuqa Depression , Tarim Basin

存在两期成藏，以喜马拉雅运动期为主；

There exist two stages of petroleum accumulation principally formed in period of Himalayan movement .

准噶尔盆地南缘喜马拉雅运动期构造应力场模拟

Numerical Simulation of Tectonic Stress Field during Himalayan Movement in Southern Margin of Junggar Basin

中新世是喜马拉雅运动的较激烈期，至上新世结束了第二幕。

The second stage started at Miocene , which was more active period , and finished at Pliocene ;

据此认为，中国华北山地的喜马拉雅运动起始于始新世，至渐新世结束了第一幕。

On North China Mountains , Himalayan movement started at Eocene and ended its first stage at Oligocene ;

喜马拉雅运动强烈的构造挤压作用造成的快速沉降和埋藏促使油气开始生成；

Rapid sedimentation and embedding by violent tectonic extrusion of Himalayan orogeny caused oil and gas to form .

分析了燕山运动和喜马拉雅运动在准噶尔盆地油气运移和聚集中的作用。

The effect of Yanshan movement and Himalayan orogeny on hydrocarbon migration and accumulation in Junggar basin is analyzed .

但自喜马拉雅运动以来，断褶构造活动强烈。

There the crustal structure was relatively stable , but folding and faulting have been intense since the Himalayan movement .

喜马拉雅运动对鄂尔多斯盆地断裂构造演化和油气藏的形成与分布具有十分重要的影响。

Himalayan tectonic movement has significant influence on the geology evolution and the oil-gas reservoir formation in the Ordos Basin .

但是，中国后海西地台遭到了后继构造运动，特别是喜马拉雅运动的破坏。

However , the post-Hercynian platforms in China have been destroyed by succeeding tectonic movements , especially the Himalayan movement .

喜马拉雅运动在塔里木盆地库车坳陷的表现&来自岩石声发射实验的证据

Expression of the Himalayan orogeny in the Kuqa depression , Tarim basin & evidence from the rock acoustic emission experiment

主要发育二叠系、三叠系、侏罗系多套烃源岩，燕山运动早期、中&晚期及喜马拉雅运动期为烃源岩的主要生、排烃高峰期。

The periods of early , middle-late Yanshan movement and Himalayan movement are its major periods for hydrocarbon generation and expelling .

喜马拉雅运动在全盆地强化了断裂的运移通道作用。

Also , the faults as channels for petroleum migration in the whole basin have been intensified by the Himalayan movement .

喜马拉雅运动：对川滇交界区古地理重建的制约和楚雄盆地的改造

Constraining of Himalayan orogeny on palinspastic reconstruction of the border area of Sichuan and Yunnan provinces and reformation of Chuxiong Basin

喜马拉雅运动使本区抬升为陆地，进一步证实晚古新世海侵边界大致在南边镇-水锅尾-基塘连线之南东地带。

Himalayan orogeny made the area uplift to continent , confirming that the late-Paleocene coast line was probably at southeast Nanbianzhen-Shuiguowei-Jitang area .

通过对已知油气藏成藏过程和圈闭形成期的分析，确定了出含油气系统关键事件和关键时期，认为海西运动期以聚油为主，喜马拉雅运动期以聚气为主；

Based on known reservoir-forming processes and trap-formed period , the critical event and critical timing for shaping a petroleum system were determined .

在琼库恰克构造带的形成和发展过程中经历了海西运动期古构造形成阶段及喜马拉雅运动期现今构造定型阶段。

The formation and development of Qongkuqak structural zone underwent two stages , i.e. , Hercynian paleostructural forming stage and Himalayan present-structural forming stage .

喜马拉雅运动期，巴楚隆起及其围斜部位则是主要的油气勘探有利区，塔东地区也值得重视。

In the Himalayan period , Bachu high and its ramp are the main favorable areas for exploration , and Tadong also deserves attention .

矿床成矿时属环太平洋成矿域的东澳大利亚成矿带，经喜马拉雅运动位移至东南亚成矿带。

The ore deposit belonged to Eastern Australia metallogenic belt during its formation , and then moved to Southeast Asia metallogenic belt by Himalayan movement .

喜马拉雅运动控制着局部构造和断裂的最后定型以及油气运移、聚集成藏。

The Himalayan movement controls final stereotype of local structures and faults , hydrocarbon migration and accumulation for forming reservoirs are also controlled by it .

喜马拉雅运动是指新生代以来的构造运动，是塔里木盆地库车坳陷构造及其圈闭形成的主要动力，对库车坳陷油气成藏起重要的作用。

Himalayan orogeny refers to the tectonic movement from Cenozoic , and it is the main power responsible for the formation of depressions and traps .