1) continent-splitting impact
大陆劈裂冲击
2) landing impact
着陆冲击
1.
Objective To quantify the response of human-chair system during landing impacts, and to testify the detecting position for system impact tests.
目的测定在固定支撑和有缓冲器支撑方式下两种假人对系统着陆冲击的响应;检验人椅系统内冲击测量位置的设置是否正确。
2.
Objective To study the characteristics of human body dynamic responses to landing impact.
方法 5名健康男青年 ,以仰卧 2 0°,承受 4～ 1 0G、5 0～ 80ms ;仰卧 30°～ 60° ,1 0G、5 0ms,半正弦脉冲的着陆冲击。
3.
Objective To study changes of human dynamic response to landing impact in selected body orientations.
目的探讨不同体位着陆冲击时人体动态响应的变化。
3) the churn boring_cleaving hole making
冲击钻劈造孔
4) continental rift
大陆裂谷
1.
They were continental rift and passive continental margin basins formed as a result of the break-up of Gondwana and the spreading of Atlantic Ocean.
西非海岸盆地群的形成和发育,与中生代以来大西洋裂开和后期的持续扩张作用有关,是冈瓦纳大陆解体和大西洋扩张形成的大陆裂谷和被动陆缘盆地。
2.
This paper deals with examples of subaerial volcanic rock-hosted copper deposits,minerogenetic series of subaerial basalt-hosted copper deposits and metallogenetie setting and hydrothermal ore-formafion in a continental rift,etc.
本文就陆相火山岩型铜矿床的实际存在，大陆玄武岩型铜矿的成矿系列，大陆裂谷的成矿环境和热液成矿作用等方面进行讨论。
3.
The basic volcanic rocks belong to continental rift tholeiite and limestone overlaid with volcanic rock and (volcani.
阿中地块南缘晚元古代索尔库里群基性火山岩与滨浅海相细粒陆源碎屑岩、成熟度较高的石英砾岩和碳酸盐岩共生,这套火山-沉积岩发生浅变质强变形作用改造,其形成于大陆裂谷构造环境,基性火山岩为大陆裂谷拉斑玄武岩,火山岩-火山碎屑岩上覆岩系碳酸盐岩中含大量小型叠层石,通过区域对比证明该套地层时代为晚元古代青白口纪,其沉积建造、岩相古地理环境与塔里木北缘库鲁克塔格地区同时代地层特征相似,说明青白口纪时南、北塔里木就有了统一的盖层。
6) continental tension rifting
大陆张裂
1.
Characteristics of the Okinawa Trough such as high heat flow values,intensive earthquake activities,volcanic activities,extensional faulting and rapid subsidence have indicated that the evolution of the trough has reached the highest stage of continental tension rifting.
高热流值、强地震活动、火山活动、张性断层作用以及快速沉降等特征表明冲绳海槽的演化已经达到了大陆张裂的最高阶段。
补充资料：标准操作冲击电压波形(见冲击电压发生器)
标准操作冲击电压波形(见冲击电压发生器)
standard switching impulse voltage waveform
b .oozhun CooZuo ChongJld，onyo boxlng标准操作冲击电压波形(standard switchingimpulse voltage waveform)见冲击电压发生器。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条