central collision

central collision的基本解释

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对心碰撞

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

When the car suffers the certain angle in front inside super-speed to hit, packing the collision in car head spreads to feel the machine spreads to feel with the safety that pack the car central part machine, can examine the car to decelerate suddenly, combine this signal in 0.01 control for inside speed delivering to safe air sac systems computer.

当汽车受到前方一定角度内的高速碰撞时，装在车前端的碰撞传感器和装汽车中部的安全传感器，就可以检测到车突然减速，并将这一信号在0.01秒之内速度传递给安全气囊系统的控制电脑。

The central problem of combination principle is how to solve the collision when component classifiers disagree.

组合原则的中心问题是当参与组合的各分类器出现不一致的情况下，如何解决这种冲突。

They are:①completed total 8 000 km long natural seismic profiles cross the northern boundary and central part of the plateau, identified several deep-cut lithospheric faults and low velocity and low density bodies under the central part of the plateau related to Cenozoic volcanic eruption, the Tarim block subducted beneath the Altun Mts;②found the evidence that the Altyn Tagh fault formed in 220～240 Ma and at least 400 km sinistral offset since, and determined quantitatively deformation in Cenozoic;③discovered 350 km long high-ultrahigh pressure metamorphic belt in the south border of the Qilian terrane,which brobably represented the Early Paleozoic boundary between the North China and Yangtze plates;④according to new discoveries of caledonian ophiolite,granite are subducted complex established paleo-collision orogenic framework of northern Qinghai-Tibet plateau;⑤proposed a new model .

本文展示了中法1995～2000年青藏高原北部地学研究的如下主要新进展：①完成8 000 km长的青藏高原北部及中部天然地震岩石圈探测剖面，确定若干条岩石圈断裂，发现与新生代火山喷发有关的青藏高原中部深处的低速、低密度体，塔里木地块俯冲于阿尔金山之下；②提出阿尔金断裂形成于220～240 Ma和左行平移400 km的科学依据及确定其新生代变形量；③确定祁连南缘350 km长的高压-超高压变质带，提出其可能代表早古生代时期北中国板块与扬子板块之间西部界限的新认识；④根据加里东期蛇绿岩、花岗岩及俯冲杂岩带的新发现，初步建立了古碰撞造山格架；⑤提出高原隆升的&地幔底辟和内向陆内俯冲&的新假设。