1) Shape evolution
波形演化
1.
Shape evolution of third-order soliton in optical fibers with quintic nonlinearity;
五阶非线性光纤中三阶孤子的波形演化
2) Waveform inversion
波形反演
1.
Comparative Study of Gauss-Newton and Gradient Waveform Inversion;
高斯—牛顿法与梯度法波形反演比较研究
2.
A genetic algorithm of body waveform inversion is presented for better understanding of crustal and upper mantle structures with deep seismic sounding waveform data.
为了更好地利用地震测深波形数据,提出了地震体波波形反演的遗传算法。
3.
Based on the broadband they waveform data within the range of 8°-38° in the Qinghai-Xizang plateau, the average velocity and its lateral inhomogeneity of upper mantle are investigated by waveform inversion.
采用波形反演方法对青藏高原地区震中距8°-38°范围内的宽频带炸波波形进行拟合，研究该地区上地幔平均速度结构以及上地幔纵、横波速度的横向不均匀性结果表明青藏高原地区的平均地壳厚度约为68km，上地幔盖层平均厚度约为30－40km，速度约为8。
3) wavelet evolution
子波演化
1.
Then, the wavelet evolution due to this geometric nonlinear effect is discussed tothus ascertaln definite physical meanings of three instantaneous data and also to of-fer a model, which can be used to separate this geometric effect from lithologic ef-fect in seismic data proces.
在此基础上讨论了这种几何非线性效应引起的子波演化，从而使三瞬资料获得了明确的物理意义，也为在地震数据处理中将这种几何效应与岩性效应的区分开提供了一个模型。
5) Dark cavity
激波演化
6) Formation and evolution
形成演化
1.
The formation and evolution of the Mega ancient lake in the middle part of the Gangdise Mountain Ranges, Xizang;
冈底斯山脉中段麦嘎古湖的形成演化发展与消亡
2.
Relationship between the formation and evolution of the South China Sea and reactivation of the Neo-Tethys;
南海的形成演化与新特提斯在南海的重新活化
3.
Its formation and evolution are closely related to development of Shicun Fault and strong subside of Lijin Sag to the north of the buried h.
结合钻井和地震资料研究纯化潜山的构造特征,精细描述了纯化潜山的构造演化过程,在此基础上探讨了纯化潜山的烃源岩、储集层、盖层以及圈闭等油气成藏条件,研究表明,纯化潜山属于典型的块断山,其形成演化与石村断层的发育及潜山北部利津洼陷的强烈下陷有着密切关系。
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