断层作用
- 与 断层作用 相关的网络例句 [注:此内容来源于网络,仅供参考]
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During later Paleogene and early Neogene, Jiyang Depression undergone from rifting activity to depression activity. During early Guantao Formation, fault active, highland eroded, slope overlapped and sags filled, and then when later Guantao Formation begin sedimented, paleotopography became plainness, new stratum overlaid all old stratum, intensity of fault activity gradually got in weaken, and developed the sedimentary system of alluvial-fluvial-freshwater shallow lake.
济阳坳陷在古近纪晚期,新近纪早期由断陷活动转为坳陷活动,经过馆陶早期的断剥超覆和填凹补平作用,到馆陶晚期古地形渐趋平缓,新地层覆盖在所有老地层之上,断层活动强度逐渐减弱,发育冲积扇-河流-淡水极浅湖沉积体系,具有良好的生储盖配置关系。
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Objective: To observe the change of regional cerebral blood flow in different region of interest under quiet condition and performing hand motor condition with single photon emission tomography, elucidate the mechanism of the brain regions activated by simple hand motor (repetitive and sequential finger- to- thumb opposition movements in turn) and detect the role of active cortical areas by analyzing the difference of rCBF in different age groups.
目的:本研究的目的是运用单光子发射断层扫描仪对比观察正常人在安静状态下和执行手指简单运动状态下脑内不同感兴趣区(region of interest, ROI)的血流量变化情况,进而阐明简单运动模式下脑内运动相关功能区的激发情况,并通过分析不同年龄组运动区激发时血流量变化的差异来探讨运动功能区的作用,对于临床中枢神经系统瘫痪后的运动功能重建和康复训练具有指导意义。
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While the current features of fault seal decide the conservation of reservoirs and heights of oil accumulations.
现今断层的封堵性则对油气的保存以及油柱高度的最终定型起到了重要作用。
- 推荐网络例句
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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.
最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。
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Only person height weeds and the fierce looks stone idles were there.
只有半人深的荒草和龇牙咧嘴的神像。
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This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.
这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。