浅海的

In neritic area,the variable period reverberation caused by seabed terrain fluctuation is the main disturbance factor to the seis- mic data quality.

在滩浅海地区，由海底地形起伏引起的变周期鸣震是影响资料品质的主要干扰因素，已有的压制海底震的方法，或多或少存在着一些不足，不能达到完全消除资料上鸣震干扰的目的。

By using the continuity equation and weak hydrody-namic interaction theory in the relaxation time approximation, the spatial variation of the radar scattering cross-sec-tion has been proved as proportional to the gradient of current velocity.

在浅海海流速度垂直分布廓线为均匀的假定下，由流体连续性方程和弛豫时间近似下流体力学弱相互作用的理论，已证明雷达散射截面的空间变化正比于海流方向上海流速度变化的梯度。

Results show that the combined technique compresses the dynamic range of submarine signal effectively and meets the demand of shallow sea dynamic range for the airborne laser bathymetry.

试验结果表明，多种方法相结合的技术可对水底信号的动态范围进行有效压缩，满足机载测深系统对浅海测量的动态范围要求；但正交偏振技术对信号测量压缩的改善效果并不明显。

In neritic area, the variable period reverberation caused by seabed terrain fluctuation is the main disturbance factor to the seismic data quality. The existing methods of suppressing seabed reverberation had some deficiencies more or less and so they cannot completely eliminate the reverberation interference.

在滩浅海地区，由海底地形起伏引起的变周期鸣震是影响资料品质的主要干扰因素，已有的压制海底鸣震的方法，或多或少存在着一些不足，不能达到完全消除资料上鸣震干扰的目的。

Any of several edible bivalve mollusks of the family Ostreidae, especially of the genera Crassostrea and Ostrea, that live chiefly in shallow marine waters and have a rough, irregularly shaped shell.

牡蛎：任一种蛎科的可食用的双壳软体动物，尤指巨蛎属和牡蛎属，主要生活在浅海水中并有坚硬的不规则形状的壳

RS has some characteristics such as speediness, synchronization, large area, high resolution and so on, it can solve many problems which are hard to overcome in traditional fathoming method.

遥感以其快速、同步、大面积及高分辨率等特点，应用在水深测量中可以解决和弥补传统方法中存在的许多难以克服的困难，给浅海水深的测量带来了极大的方便。

Five pieces of paleogeographic maps were made out with modern stratigraphic principles and sedimantary system method. It is shown by the maps that in the beginning of the Changzhougou time the Yanshan Region was occupied by alluvial environment with paleoriver flowing northeast, in the middle of the Changzhougou time a transgression changed whole Yanshan Region into shoreline-shallow sea environment gradually, and sedimentary boundary extended so continuously that by the Gaoyuzhuang time it had overpassed far beyond the Yanshan Region.

在缺乏良好等时面的情况下，本文依据现代地层学原理和沉积体系分析法编制了常州沟组初期与中期，串岭沟组初期，大红峪组初期，及高于庄组初期燕山地区的岩相古地理图，示意了燕山地区在长城纪时由冲积扇-河流为主的陆地环境向滨海-浅海环境的演变过程，并揭示了沉积区域不断扩大的趋势，表明常州沟组初期，以蓟县-宽城为轴线发育了冲积相组，海岸线可能在燕山以北，常州沟组中期发生海侵，沉积区扩大至整个燕山地区，大红峪组时海盆范围继续扩大，高于庄组时，沉积边界已远远超出燕山地区。

The deep formations in the Tertiary,pre-Tertiary,littoral areas and offshore will be the most favorable exploration fields in the basins of the eastern area in North China for 21st century.

在该地区应着重研究多勘探层系、勘探程度的差异性和地质理论的新进展，充分挖掘各探区内各单元的油气资源潜力，第三系深层、前第三系、滩海和浅海应是华北东部盆地21世纪油气勘探的重点领域。

Inunderwater acoustic research specially in shallow-sea acoustic,the scatteringon different rough surface is important factor affecting underwater environmentand background.

粗糙表面声散射在很多领域均有重要的应用，水声研究中尤其是浅海声学的研究，各种粗糙界面的散射更是影响水下环境和背景的重要因素。

REE geochemical characteristics and their systematic changes in the sedimentary section suggest that there existed a process of ingression-regression in this area in the early Cambrian period. The black shale series resulted from the mixing between normal seawater sediments and hot seawater sediments and were deposited under the transitional condition from reduction to semi-reduction and weak oxidation in a shallow-sea clinoform zone of a relatively deep sea environment with dry climate.

稀土元素地球化学特征反映该区早寒武世曾发生过一次明显的海侵-海退过程，黑色岩系为正常海水与热水混合沉积的产物，形成于缺氧还原状态过渡到半还原-弱氧化状态的过程中，沉积环境为干燥气候条件下相对较深的浅海斜坡环境。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。