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seafloor相关的网络例句

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与 seafloor 相关的网络例句 [注:此内容来源于网络,仅供参考]

Batfish are poor swimmers, preferring to use their strangely adapted pectoral fins like legs to crawl about the seafloor.

蝙蝠鱼是可怜的游泳者,更喜欢用它们的奇妙的适合的胸鳍像脚爬行大约在海底。

By electromagnetic theory, for the case that the magnetic dipole source and the receiver are set in seawater, the general expressions of frequency_domain electromagnetic responses for a layered benthal model are deduced. From those, the transient response expressions of three common configurations—vertical magnetic dipole_dipole, central loop, and coincident loop, located on the surface of uniform half_space seafloor, are derived respectively, supposing that seawater is uniform half space, or its depth is finite.

根据电磁场理论,推导了磁偶源和接收点均位于海水中时层状海底模型的频域电磁场响应一般表达式,并通过此式,得到了海水为均匀半空间和有限海水深度两种情况下,垂直磁偶极装置、中心回线和重叠回线分别置于均匀半空间海底表面时的瞬变电磁响应表达式。

In order to obtain a more accurate prediction of intersection between the temperature gradient measured at sub-seafloor and the gas hydrate phase boundary curve i.e.

为了能更准确的求得天然气水合物稳定生成的底部,即海床的地温梯度与天然气水合物稳定曲线的交点。

Clinochlore, illite and quartz were found to be in different depths of the seafloor sediments using the X-ray diffraction analysis. In addition, by use of the SEM observation, no biogenic minerals were found.

本研究以 X-ray 绕射分析海床沉积物中的矿物,每个深度的样品皆发现有 Clinochlore, Illite, Quartz 等矿物,再经 SEM 的观察都没有发现生物源矿物。

BGHS;Base of Gas Hydrate Stability, we attached 5 miniature temperature probes to the outside walls of a sediment corer to measure the temperature and thermal gradient of sub-seafloor when taking a core sample.

为了能更准确的求得天然气水合物稳定生成的底部,即海床的地温梯度与天然气水合物稳定曲线的交点。我们将5根小型温度探针系绑於岩心采样器之外管壁上,在岩心采样时同时量取海床底下之温度。

This theory is demonstrated by three examples: the natural gas blowout when drilling in the permafrost, the hydrate cropouts in the seafloor and the gas bubbles in abyssal plumes. Then, several conclusions are drawn: there maybe exist the seeping and diffusing types of gas hydrate reservoirs which may still be growing in the Xisha trough, Dongsha continental slope of the South China Sea, west and south of Taiwan basin, and Bijianan basin; whereas in the Qiangtang basin of the Qinghai\|Tibet plateau may exist the regressive\|type gas hydrate deposit. Furthermore, the phenomenon of hydrocarbon gas leaking in the Qilian mountain areas and Junger basin indicates that these areas may ensconce gas hydrate reservoirs.

指出天然气水合物赋存状态主要有3种类型,即成长型、成熟型和消退型,认为我国南海北部陆坡区的西沙海槽、东沙群岛东南坡、台西南盆地、笔架南盆地等区域有可能存在着仍处于发育阶段的渗透型或扩散型水合物层,而青藏高原羌塘盆地则是属于消退型水合物,祁连山地区、准噶尔盆地等的烃类气体泄漏表明在我国西北和东北的冻土带也可能存在着含气水合物层。

Based on the survey data in recent years, there are five micro-morphological feature parts in the sea bed of Chengdao area, including erosion morphology, sliding extrusion ridge and collapse, remained scarp or monadnock, blocky seafloor, rough and smooth seafloor, etc.

根据多次的调查资料分析,埕岛海域现在的海底上主要存在5种微地貌形态区即冲蚀地貌区、滑动挤压脊和塌陷凹坑地貌区、侵蚀残留岗丘或台地、斑状海底地貌区、粗糙和平滑海底。

The analysis of the basic knowledge of geothermic field of natural gas hydrate reservoir regions in seafloor indicates that it is feasible to establish the basic geothermic field model of natural gas hydrate reservoir regions in seafloor following the theory and method of basin geothermic model.

在分析海底天然气水合物赋藏区域地热场特征的基础上,借鉴盆地地热模型理论和方法,建立了海底天然气水合物赋藏区域的地热基本模型,并详细介绍了边界条件和导热系数的确定方法。

Seafloor experiments suggest that the real-time cascade decimation technique is efficient method in collection of information for seafloor resource exploration.

经海试检验证实,本文所提出的实时级联分样技术为海底以下的资源探测提供了一种有效的信息提取手段。

Marine gas seepage not only influences the physical properties of the seafloor sediments, but also significantly alters the geomorphology of the seafloor, such as the occurrence of pockmarks, mud volcanoes, authigenic carbonate and cold seep communities on seafloor.

海底天然气渗漏可以指示沉积层中的烃类聚集带,渗漏出的大量气体可能影响全球的气候变化,此外,与海底渗漏相关的浅层气改变了海底沉积物的土工性质,可能对海底工程构成威胁。

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