1) integral trace
积分道
1.
Furthermore, the relationship between integral trace and absolute velocity is given in this formula, which has more pr.
改进后的公式也揭示了积分道 (对反射系数的积分 )与绝对速度的关系 ,更有实用价值 。
2) trace integration method
道积分法
1.
It is possible to predict coal seam thickness with trace integration method,but the type and dominant frequency of wavelet have an effect on the calculated coal seam thickness.
道积分法反演煤层厚度，其计算的煤层厚度往往受到地震子波的类型和主频的影响。
3) trace integration
道积分
1.
Interpretation of thin interbeds in trace integration section and modeling of three-dimensional petrophysical parameter volume;
道积分剖面薄互层特征解释及三维地质物性参数体模拟
2.
From the view of the foundational theory of thin bed reflection and model study, the paper introduceds the quantitative interpretation method for the thin bed thickness in trace integration section, and calculates the thickness of coal seam using the model and practical data.
从薄层反射的基础理论和正演模型研究的角度出发，给出了道积分剖面的薄层厚度定量解释方法，并利用正演模型和实际资料进行了煤层厚度的反演计算，证明了该方法的可行性和实用
4) trace integral
道积分
1.
The trace integral method and the relative interval velocity inversion using Walsh function are theoretically comparied.
对地震道积分法和沃尔什（Ｗａｌｓｈ）函数相对层速度反演法，从方法、处理结果和地震解释等方面进行了比较和分析，并用这两种方法处理了层状模型数据和实际地震资料。
2.
Relative poisson s ratio analysis technique is developed based on trace integral principle and AVO attribute analysis technology according to the special condition of the gas reservoirs.
针对这一特殊气藏条件,利用道积分原理和AVO属性分析技术,开发了相对泊松比分析技术,找出了相对泊松比与气藏之间的特征关系,建立了中深层砂岩气藏的检测方法。
5) Integral Trajectory
积分弹道
6) Contour integration
围道积分
1.
On evaluating∫integral from n=-∞ to +∞(e~(ax~2+bx)dx)by contour integration;
运用围道积分计算∫integral from n=-∞ to +∞(e~(ax~2+bx)dx)
2.
Contour integration by Cauchy integral formula formula is used.
提出了利用围道积分由Cauchy积分公式计算常系数线性常微分方程的基解矩阵的方法 ,比以往的方法更为简洁明
3.
By contour integration we show that |(?),q〉_* is the common eigenvector of e~(-iφ)and the photon number difference operator.
找到了双模场中Susskind-Glogower相算符e~(iφ)态矢|,q〉的对偶本征矢|,q〉_*,运用围道积分证明了|,q〉_*是e~(-iφ)和光子数差算符的共同本征矢。
补充资料：道-道间寻道时间
道-道间寻道时间(single track seek)：
指磁头从一磁道移动至另一磁道的时间，单位为毫秒(ms)。
指磁头从一磁道移动至另一磁道的时间，单位为毫秒(ms)。
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