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1)  long cable and deep reflection seismic data
长电缆深反射地震
2)  long cable seismic
长电缆地震
1.
Therefore,Moho behavior in the depression can be revealed by the long cable seismic section.
横切渤中凹陷的长电缆地震剖面长约100km,记录时间达14s,探测深度超过莫霍面深达地幔。
3)  Deep seismic reflection
深反射地震
1.
Seismic migration is a main tool to improve horizontal resolution of the deep seismic reflection data.
本文从偏移的基本原理出发,阐述了一些在设计数据采集参数时应注意的问题,并根据深反射地震资料的一些特点,讨论了深反射地震数据偏移处理中的几个问题,给出了两个应用实例。
2.
Since then many other countries have carried out deep seismic reflection researches.
介绍了深反射地震技术的发展与应用状况。
3.
International geologists have recognized deep seismic reflection as high technology in probing fine structure of lithosphere.
当前探测深部构造的地球物理技术主要是地震学的方法,其中的深反射地震技术目前被国际地学界公认为探测岩石圈精细结构的高技术。
4)  deep reflection seism
深反射地震
1.
The key to the processing of deep reflection seismic data seems to be the cxtraction and enhancement of deep weak effective signal from the disturbing background, thus arising the signal-to-noise ratio and resolution ratio of the profile.
深反射地震资料处理的关键是从干扰背景中提取和增强深层弱有效信号,提高剖面的信噪比和分辨率。
2.
The present paper has dealt systematically with a practical and effective deep reflection seismic technique—small-scale wide line reflection seismic technique.
深反射地震方法分辨率高、准确可靠 ,是用于地学研究的一种有效方法技术。
5)  Deep seismic reflection
深地震反射
1.
The basin-range junction zone has complex surface geological conditions and a rather undulate tomography,where deep seismic reflection data are characterized by a low S/N ratio,strong multifold noises and great lateral variation in velocity.
盆山结合带地质条件复杂、地形起伏大,深地震反射资料具有信噪比低、各种干扰波严重以及速度横向变化大等特点。
2.
Deep seismic reflection profiling across Jiashi strong earthquake swarm region has revealed fine crustal images through to M-discontinuity of the studied area.
穿过伽师强震群的深地震反射剖面提供了研究区从地表直至莫霍界面的地壳细结构图像。
3.
The mid-crustal reflection formed by the Main Himalayan Thrust (MHT)is interpreted to be underthrust gradually northward beneath the crust of southern Tibet by intensive processing of the data of two N-S-trending deep seismic reflection profiles on the southern side of the Yarlung Zangbo River obtained by Project INDEPTH II in 1993.
通过对INDEPTHII在雅鲁藏布江南的2条南北向深地震反射剖面资料的进一步处理,观察到主喜马拉雅逆冲断裂带(MHT)形成的反射向北逐渐倾没于藏南地壳之下。
6)  Seismic deep reflection
地震深反射
1.
Results of seismic deep reflection,high resolution refraction and shal- low artificial seismic exploration indicate that the fault on the northern bank of the Weihe river is composed of two branches:one is the Yaodian-Zhangjiawan fault and the other is the Chuanzhang-Zuitou fault.
地震深反射、高分辨率折射和浅层人工地震探测结果表明,渭河北岸断裂由两条断层组成:一条为窑店—张家湾断层,另一条为船张—咀头断层。
补充资料:深反射

  
  深反射
  〖HT5”SS〗deep reflex

  是刺激肌腱而引起的牵张反射,其反射弧包括肌腱的感受器、感觉神经元、脑干或脊髓的中间神经元、运动神经元和肌肉。
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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