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sinistral相关的网络例句

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与 sinistral 相关的网络例句 [注:此内容来源于网络,仅供参考]

In experiments,an injectionchanges the pattern of sinistral eggs,(80) does not influence dextral eggs.

在实验中,用取自右旋卵子的细胞质进行的注射,可改变左旋卵子的模式;用取自左旋卵子的细胞质进行的注射却不能影响到右旋卵子

Changes the pattern of sinistral eggs,(80) does not influence dextral eggs.

左旋卵子的模式;用取自左旋卵子的细胞质进行的注射却不能影响到右旋卵子

However, some broods possess a few snails of the opposing hand, and in predominantly sinistral broods, the incidence of dextrality is surprisingly high.

一些窝中会有一些相反旋向的蜗牛,而780。且在主要是左旋的窝种,781。出现右旋的几率是令人惊奇的高。

However, some broods possess a few snails of the opposing hand, and in predominantly sinistral broods, the incidence of dextrality is surpri singly high.

可是,一些窝中会有一些相反旋向的蜗牛,而且在主要是左旋的窝种,出现右旋的几率是令人惊奇的高。

Tern of sinistral eggs,but an injection from sinistral eggs does not influenc

子的细胞质进行的注射却不能影响到右旋卵子。

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。

Based on technical processing of high-resolution SPOT images and aerophotos, detailed mapping of offset landforms in combination with field examination and displacement measurement, and dating of offset geomorphic surfaces by using carbon fourteen (14C), cosmogenic nuclides (10Be 26Al) and thermoluminescence methods, the Holocene sinistral slip rates on different segments of the Altyn Tagh Fault are obtained. The slip rates reach 17.5 mm/a on the central and western segments west of Aksay Town, 11 mm/a on the Subei—Shibaocheng segment, 4.8 mm/a on the Sulehe segment and only 2.2 mm/a on the Kuantanshan segment, a easternmost segment of the ATF. The sudden change points for loss of sinistral slip rates are located at the Subei, Shibaocheng and Sulehe triple junctions where NW-trending active thrust faults splay from the ATF and propagate southeastward.

在高分辨率SPOT卫星数字影像和大比例尺航片处理、断错地貌制图、野外核实与位移测量基础上,利用宇宙成因核素(10Be、26Al)、碳十四(14C)和热释光等多种测年手段,厘定了各断错地貌面的形成年龄,得到了阿尔金断裂带不同段落全新世左旋走滑速率:阿克赛以西的中、西段左旋走滑速率可达17.5 mm/a,肃北—石包城段为11 mm/a左右,疏勒河口段减少到4.8mm/a左右,东端宽滩山段仅约2.2 mm/a,左旋走滑速率突变点位于阿尔金断裂带中东段存在分支活动逆断层向南东扩展的肃北、石包城和疏勒河等三联点上。

In experiments ,an injection of cytoplasm from dextral eggs changes the attern of sinistral eggs ,but an injection from sinistral eggs does not infl uence dextral eggs .

在实验中,用取自右旋卵子的细胞质进行的注射,可改变左旋卵子的模式;用取自左旋卵子的细胞质进行的注射却不能影响到右旋卵子。

The Altun fault, a famous tremendous sinistral strike-slip fault in NW China, is composed mainly of the Altun,master fault several secondary subhorizontal, sinistral, strike-slip faults and oblique faults.

阿尔金走滑断裂带主要由阿尔金主干断层与几条近于平行的左行走滑断层和斜交断层组成,其空间分布规律可用左行走滑简单剪切模型解释。

The shearing and E-dip lineations of the plutons near the Shangdan subduction zone proves that the zone underwent thrust→thrust-sinistral shear→sinistral slip, revealing the lateral move and elevation of the core complex from the deep to low levels and a dynamic evolution of oblique subduction-collision.

商丹构造带边缘花岗岩体左行剪切及东倾伏的拉伸线理证实,商丹带经历了逆冲→逆-左行→左行三个阶段的递进演化,为秦岭杂岩相对由深部到浅部向西侧向运移抬升的认识提供了坚实依据,并揭示了一种斜向俯冲—碰撞的运动学、动力学演化过程。

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