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fault movement相关的网络例句

查询词典 fault movement

与 fault movement 相关的网络例句 [注:此内容来源于网络,仅供参考]

If the relative movement of hanging wall and footwall is parallel to the strike of fault plane, it is a strike slip fault.

如果断层上盘和下盘的岩石相对位移运动是平行断层面走向的,这种断层称为走滑断层。

Along the Daqingshan Piedmont Fault exist typical tectonic landforms, which are fault scarp, 3 orders of piedmont terrace, 5 orders of river terrace and 3 orders of alluvial fan, all carefully dated and measured. All these landforms display the intense vertical movement of this fault.

沿大青山山前断裂发育典型的构造地貌,计有夷平面、3级山前台地、5级河流阶地和3期洪积扇,基岩断层崖和全新世断层陡坎分布广泛,标志着断裂强烈的垂直差异性升降运动和间歇性活动的特点。

Wuxia area was located on the eastern of northwest Junggar basin, it was a zone of bruchfalten affected by multiphase tectonic activity, have many faults and its fold morphology were very complicated, underwent three large structural activities, which happened in the late Hercynian movement, Indo-Chinese movement, and the Yanshan movement, by this,strata of Wuxia area can be divided into two primary tectonic sequences and seven secondary tectonic sequences, on plane, Wuxia area can be divided into three secondary structural units from north to south,they are foreland thrust belt, Wuxia fault fold belt and monocline belt, further, from west to east Wuxia fault fold belt can be divided into four fault fold belts.

乌夏断裂带位于准噶尔盆地西北缘冲断带东段,是一个受多期构造叠加影响的断褶带,断裂发育,褶皱形态复杂,自成盆期以来经历了海西、印支、燕山和喜马拉雅等多期构造运动,可划分为2个一级构造层序和7个亚构造层序,可划分出山前冲断带、乌夏断褶带、南部单斜带三个次级构造单元和四个更次一级的构造单元。

This movement occurs along fault lines of different types. The San Andreas Fault is one of them. The sudden displacement along the fault, in 1906, produced the great San Francisco earthquake.

这种移动造成了不同类型的断层,San Andreas断层就是其中之一。1906年断层的突然运动造成了旧金山大地震。

Combined the geological analysis with analogue modeling experiments,the evolution of the Yinggehai basin could be divided into four main stages:(1) Before 42Ma,controlled by the southeastward extension of the Beibu Gulf basin on the northern continental margin,the Yinggehai basin experienced dextral pull-apart.Bounded by NS-trending Yingxi fault,the transtensional areas mainly are the northwest part and along the eastern boundary of the basin.(2) From 42 to 21Ma,the development of the main rift body in Yinggehai basin was mainly controlled by the southward slip and clockwise rotation of the Indochina block along the Red River fault zone,and the sedimentation was strengthened due to the sinistral transtension.In the east,the subsidence is deepened due to the dextral transtension.(3) From 21 to 10.4Ma,the sinistral movement of the Indochina block slowed down to still.From 21 to 15.5Ma,the northwest part of the basin began to inverse locally because of post-rift thermal subsidence of the whole basin.(4) From 10.4Ma to present,the basin was affected by the dextral movement of the South China block along the Red River fault zone and thermal accident in a new phase at 5Ma.

结合地质分析和物理模拟实验,莺歌海盆地的演化大致可以分为以下4个主要阶段:早期(42 Ma以前)主要受到南海北部陆缘裂解造成的右旋转换伸展作用的影响,但影响范围较小,主要为莺歌海盆地西北部和东部边界。42~21 Ma期间,主要受控于印支地块左行走滑和顺时针旋转作用的影响,莺歌海盆地在此期间发育了主体裂陷体系,东侧受到右旋转换伸展应力场的叠加影响而导致沉降加强;21~10.4 Ma期间,受印支地块逐渐减弱直至停止的左行走滑作用的影响,盆地西北部在21~15.5 Ma期间发生局部反转褶皱,但盆地整体进入以热沉降为主的时期;10.4 Ma以后,盆地受华南地块沿红河断裂右旋走滑作用和5 Ma以后新一期热事件的影响。

Yizheng movement, Wubao movement and Sanduo movement happened ordinally in Gaoyou depression and then regional unconformity formed. According to the feature of unconformity and stockwerke, the sedimentary cover could be compartmentalized as upper, middle and subjacent stockwerke. Fault activity is different because of different intensity of structural movement.

高邮凹陷先后经历了仪征运动、吴堡运动和三垛运动等几大规模构造运动,形成了区域性不整合面,依据不整合及其分隔的构造层的结构特点,可将高邮凹陷的沉积盖层划分为上、中、下三个构造层。

According the spatial correlation, it is believed that the Jintananshan Fault as well as the whole fault bundle is the eastward-extending part of the Altun Fault. The special modality of the fault bundle, which spreads out eastwards, is in favor of decomposing and absorbing the slip movement, which is normal at a strike-slip fault's ends.

分析认为金塔南山断裂以及整个阿拉善南缘断裂束是阿尔金断裂左旋运动的东延部分,断裂束在平面上&帚状&的、向东撒开的构造样式有利于走滑运动量的分解、消减和吸收,符合走滑断裂末端的构造特点。

Seismographic records showed that the seismic waves produced by the fault movement were much less energetic than those produced directly by the nuclear explosion.

测震记录显示断层运动产生的震波远比核爆直接产生的震波来得弱。

This suggests the incomplete welding of the sides of the fault by the granitic intrusion along it,which afterwards permitted the reactivation of the fault,probably due to the relatively independent movement of the faulted blocks,as a dextral transcurrent fault.

这意味着稍早的花岗岩侵入体冷凝冷却并没有完全焊接地壳内一些大尺度断层,地壳断块的相对独立活动可以造成沿着这些断层发生与区域变形场不协调的右行走向滑动,进而形成岩墙群弧形展布所需要的地应力场。

A important feature in research region is: synsedimentary motion of faults result fault block"tilting movement"and change hydrocarbon migration direction as well as forming fault-bock trap in the center of resource rock, This is favorable for fault-block traps to accumulate hydrocarbon.

本区的另一个重要特征是断裂同沉积活动引起的掀斜运动改变了区域油气运移的方向,在烃源岩发育的沉积中心形成掀斜断块构造圈闭,有利于油气的聚集。

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