seismic motion

seismic motion的基本解释

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地震活动, 地震运动

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

The principles are as follows:①preliminary interpretation is carried out on crosswell seismic data in depth domain to establish an accurate velocity model;②sinc interpolating function is used in depth-time conversion to realize waveform fidelity;③the recognition of surface seismic data is utilized to ascertain the reflection characteristics of crosswell seismic data in time domain;④ good spatial continuity of surface seismic data is adopted to retrieve the "hopper" defect in crosswell seismic profiles and the deficiency of lateral contrast between crosswell seismic data;⑤in fine calibration of well-side traces of crosswells and surface seismic data, coincident time-depth relation is used to match two seismic data so as to make the calibration more reasonable;⑥in multi-crosswell seismic data inversion by sparse spike inversion method, lateral restraints are strengthened to ensure the continuity of inversed wave impedance profile.

实现反演的基本原理是：对深度域井间地震资料进行初步解释；建立精确的速度模型；在对井间地震剖面进行深时转换时采用sinc插值函数实现波形保真；利用对地面地震资料的认识来落实时间域井间地震资料的反射特征；利用地面地震资料良好的空间连续性弥补井间地震剖面的"漏斗"缺陷和井间资料之间横向对比性的不足；在井间地震和地面地震井旁道精细标定中，通过一致的时深关系来实现两种地震资料之间的匹配，使井旁道的标定更加合理；在利用稀疏脉冲反演方法进行连井井间地震资料反演时，通过增强横向约束保证反演波阻抗剖面的连续性。

1Based on the characteristics of carbonatite reservoir in Sangtamu area, we summarize the type of seismic reflection and the distribution of oil and gas.(2)Through the study of the lateral difference of local amplitude, which can predict the short, unorderly reflective energy gobbet of carbonatite reservior, we study the distribution of carbonatite reservoir with crack.(3)Analyzing the change of the seismic waveform, applying nerve network method to classify the seismic waveform, find the rule of its change, recognizing the change rule of seismic facies.(4)Applying the seismic multi-attribute cross method to study the surface and inner of carbonatite reservoir in buried hill. We first extract the 5 kinds of seismic attribute. Through a series of choices, we find those seismic attributes that are sensitive to the change of carbonatite reservoir.

主要的研究包括：①根据桑塔木碳酸盐岩的储层特点，总结了该区的地震反射特征及油气分布特征；②研究出一种有针对性的地震属性--局域振幅横向差异性，来定量刻画潜山内部"短轴"杂乱反射能量团，预测缝洞型碳酸盐岩内部储层的平面分布规律；③通过对地震波形变化的分析，运用神经网络对地震波形进行有效分类，找出波形变化的总体规律，从而认识地震相的变化规律；④应用交会法地震多属性分析方法，对潜山表层和内部分别提取了5大类40种地震属性，通过一系列分析表层及内幕各自优选出3种、4种地震属性用于进行交会分析。

Based on the special geological traits of the fourth member of the Shahejie Formation of Block Tuo-123 in Dongying Depression, in combination with the sequence identification and comparison of the seismic section, five typical seismic facieses were summarized, including sub-parallel sheeted seismic facies, hummocky onlap fill seismic facies, lens seismic facies, wedge seismic facies and blank seismic facies, and their traits and distribution range were analysed.

针对东营凹陷坨123断块沙四段的具体地质背景，在对地震剖面层序划分和追踪对比的基础上，总结出5种典型的地震相：亚平行席状地震相、丘形上超充填地震相、透镜状地震相、楔形杂乱地震相和空白地震相，并分析了其主要特征及展布范围。

与seismic motion相关的网络解释 [注：此内容来源于网络，仅供参考]

seismic origin：地震成因

seismic motion 地震活动; 地震运动 | seismic origin 地震成因 | seismic phase 震相

slow motion：慢镜头

TBBA街球教学之慢镜头(Slow Motion)与 TBBA街球教学之慢镜头(Slow Motion) 不相关的其它视频TBBA街球教学之慢镜头(Slow Motion) 视频其他来源视频名称: TBBA街球教学之慢镜头(Slow Motion)视频描述: TBBA街球教学之慢镜头(Slow Motion)

Seismic activity：地震活动; 地震活动性

seismic acceleration indicator 地震加速指示计 | seismic activity 地震活动; 地震活动性 | seismic amplifier 地震放大器