interbedded

简明释义

英[ˌɪntəˈbedɪd]美[ˌɪntərˈbedɪd]

adj. [地质] 层间的；夹层之间的

英英释义

单词用法

同义词

反义词

例句

1.This method of three-dimensional integrated modeling is suitable for thin interbedded sand-mud projections.

此三维综合建模的方法比较适合砂泥薄互层的预测。

2.PDC bits have been used to drill the homogeneous formation from soft to medium-hard, but they are not suitable for drilling in gravel and multi-interbedded formation.

PD C钻头用于软到中硬的均质地层钻进具有钻速高、寿命长等特点，但不适合含砾石地层和软硬交错地层。

3.Low compressive strength of soft to medium formations. Such as soft shale, soft limestone, soft sandstone, hard and soft abrasive interbedded medium formation.

低抗压强度的软到中等地层，如中软页岩。中软石灰岩。中软砂岩。和软硬研磨性夹层的中等地层。

4.Hot event deposits occurred in Liantuo Formation of Lower Sinian, interbedded in fluvial facies sandstones and siltstones.

热事件沉积产物见于下震旦统莲沱组，夹于河流相沉积的砂岩及粉砂岩中。

5.A shale formation with sandstone interbedded is also a potential oil bearing formation.

以泥岩为主，夹砂岩的地层也可能是油气层。

6.Major sedimentary facies in the Huanhe-Huachi Formation include lacustrine facies, delta facies, meandering fluvial facies, and interbedded eolian sandstone facies.

而在环河华池组主要沉积了湖相、三角洲相、曲流河相及风成砂岩夹层。

7.The dynamic characteristic of interbedded soil is similar to that of soft soil; and this property is caused by its special conformation, i. e. the feeble horizontal joint planes are overgrown.

初步分析结果表明：互层土具有软土的动力特性，这主要是由互层土的特殊物理构造造成的，即在互层土中存在很密的水平薄弱面。

8.The presence of interbedded 交错沉积 volcanic ash layers can help date the surrounding rock formations.

交错沉积的火山灰层的存在可以帮助确定周围岩层的年代。

9.The interbedded 交错沉积 layers of limestone and clay indicate varying depositional conditions over time.

石灰岩和粘土的交错沉积层表明随着时间的推移，沉积条件发生了变化。

10.The geological survey revealed that the region contains layers of sandstone and shale that are interbedded 交错沉积.

地质调查显示，该地区包含交错沉积的砂岩和页岩层。

11.Geologists often analyze interbedded 交错沉积 materials to understand tectonic activity in the area.

地质学家通常分析交错沉积的材料，以了解该地区的构造活动。

12.In the study of sedimentary rocks, we often encounter interbedded 交错沉积 formations that provide insight into past environments.

在沉积岩的研究中，我们经常遇到交错沉积的地层，这为了解过去的环境提供了线索。

作文

The earth's geology is a complex tapestry of various layers and formations that tell the story of our planet's history. One of the fascinating features found in sedimentary rock formations is the concept of interbedded layers. These layers are characterized by the alternating deposition of different types of sediments, such as sandstones, shales, and limestones, which can provide valuable insights into the environmental conditions that prevailed during their formation. For instance, when we observe a sequence of rocks that are interbedded, it often indicates changes in sediment supply or shifts in depositional environments over time. Understanding interbedded formations is crucial for geologists, especially when exploring natural resources like oil, gas, and groundwater. The presence of interbedded layers can significantly affect the permeability and porosity of a geological formation, influencing how fluids move through the subsurface. In some cases, these interbedded layers can act as barriers to fluid flow, while in others, they may enhance the storage capacity of reservoirs. Therefore, studying the characteristics of interbedded layers helps in predicting the behavior of these resources and planning extraction methods effectively.Moreover, interbedded formations also hold paleontological significance. Fossils found within these layers can provide clues about the ancient ecosystems that existed millions of years ago. By analyzing the types of fossils and their distribution within the interbedded layers, scientists can reconstruct past environments and understand the evolutionary processes that shaped life on Earth.The formation of interbedded layers typically occurs in settings where there are fluctuations in sedimentation rates or changes in energy conditions. For example, in a river delta, periods of high flow might deposit coarse sediments, while calmer conditions could allow finer materials to settle. This results in a stratified sequence of rocks that are interbedded with varying grain sizes and compositions. Similarly, marine environments can produce interbedded sequences as a result of changes in sea level or water temperature, further illustrating the dynamic nature of Earth’s processes.In conclusion, the study of interbedded layers provides a window into the geological past, revealing the interplay of various environmental factors that have shaped our planet. From resource exploration to understanding ancient life, the significance of interbedded formations cannot be overstated. As we continue to explore and learn about Earth’s geology, the concept of interbedded layers will remain a key area of focus, helping us to piece together the intricate puzzle of our planet's history.

地球的地质是一个复杂的图案，由不同的层和构造组成，讲述着我们星球的历史。其中一种在沉积岩层中发现的迷人特征是交互层的概念。这些层的特点是不同类型沉积物（如砂岩、页岩和石灰岩）的交替沉积，这可以提供关于其形成时环境条件的宝贵见解。例如，当我们观察到一系列交互层的岩石时，通常表明沉积供应的变化或沉积环境随时间的变化。理解交互层的构造对地质学家至关重要，特别是在勘探天然资源（如石油、天然气和地下水）时。交互层的存在可能会显著影响地质构造的渗透性和孔隙度，从而影响流体在地下的运动。在某些情况下，这些交互层可能会作为流动的障碍，而在其他情况下，它们可能会增强储层的存储能力。因此，研究交互层的特征有助于预测这些资源的行为并有效规划开采方法。此外，交互层的构造也具有古生物学意义。在这些层中发现的化石可以提供关于数百万年前古生态系统的线索。通过分析化石的类型及其在交互层中的分布，科学家可以重建过去的环境，并理解塑造地球生命的进化过程。交互层的形成通常发生在沉积速率波动或能量条件变化的环境中。例如，在河口三角洲，高流量时期可能会沉积粗颗粒沉积物，而较平静的条件则可能允许细颗粒物质沉降。这导致了不同粒径和成分的岩石层次交替出现，形成了交互层。类似地，海洋环境也可能由于海平面或水温的变化而产生交互层序列，进一步说明了地球过程的动态特性。总之，研究交互层为我们提供了一个了解地质过去的窗口，揭示了塑造我们星球的各种环境因素之间的相互作用。从资源勘探到理解古代生命，交互层构造的重要性不容小觑。随着我们继续探索和学习地球的地质，交互层的概念将始终是一个关键关注领域，帮助我们拼凑出我们星球历史的复杂拼图。