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Brain signal source localization is a process of inverse calculation from electroencephalogram signal.

脑电源定位是根据头皮观测电位进行逆问题计算的过程。

Based on the 3-D acoustic equation and Tarantola′s generalized inversion theorem, taking into consideration the character of cross-well survey, a 2.5-D cross-well waveform tomography method in the frequency domain is presented here.

从频率域3-D声波波动方程出发,结合井间观测方式的特点,基于Tarantola广义反演理论,提出了一种频率域2.5-D井间波形层析成像方法。

All of these are very significant in the study of ionosphere space weather.

这对于电离层空间天气观测研究具有重要的意义。

A case study showed that it is feasible to estimate the ionospheric irregularity drifts with this method.

实例分析与计算结果表明,利用单站多卫星观测估计电离层不规则结构漂移是一种合理可行的方法。

Ionospheric physics is considered as an experimental science.

电离层物理学是一门以观测为基础的实验科学。

In chapter 4, the experimentation of incipient cavitation in a transparent jet pump has been done and the data is computed.

第四章对透明射流泵的初生空化作了试验观测和数据计算研究。

The in situ visualization of pyrolysis of kerogen and asphalt in high-temperature and high-pressure water studied by hydrothermal anvil cell.

采用热液对顶砧压腔装置,对高温高压水中干酪根和沥青质的热解过程进行了原位观测。

An alternative approach is to start from observational data and to reconstruct corresponding theoretical Lagrangian.

另一种方法是从观测数据出发去构造相应的拉氏量。

Datong Hydrometric Station and Sediment Monitoring Profile are located in the landward limit of the Yangtze Estuary.

大通水文站和泥沙观测断面位于长江河口的上边界。

This work is one part of the research of the larynx dynamic observing and analyzing system.

本研究是"喉动态观测分析系统"研究工作的一部分。

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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。

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。

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。