interbedding

简明释义

英[/ˌɪntərˈbɛdɪŋ/]美[/ˌɪntərˈbɛdɪŋ/]

n. 互层，中间层

v. 埋于隔层之间（interbed 的 ing 形式）

英英释义

单词用法

同义词

反义词

例句

1.The interbedding natures exist not only between red sandstone, mudstone and shale but also between red beds with coal seam, magmatite, evaporite and varied rock, respectively.

由于砂岩、泥岩、页岩、蒸发岩、杂色岩等多种软硬岩层互层结构和工程活动等因素的影响，沿着软弱结构面易发生滑坡、差异风化等工程地质问题。

2.In recent years, lots of reservoirs of thin sand and mudstone interbedding in Kailu area have high output.

而在开鲁等地区存在大量的砂、泥岩薄互层油气藏，近年来产量比较可观。

3.Moreover, episodic activities of the growth faults changed the sedimentary environment and resulted in the interbedding of witherite and barite ores.

同生断裂的幕式活动，引起沉积环境的改变，形成了毒重石和重晶石的互层。

4.The interbedding natures exist not only between red sandstone, mudstone and shale but also between red beds with coal seam, magmatite, evaporite and varied rock, respectively.

由于砂岩、泥岩、页岩、蒸发岩、杂色岩等多种软硬岩层互层结构和工程活动等因素的影响，沿着软弱结构面易发生滑坡、差异风化等工程地质问题。

5.The interbedding of different minerals can create unique geological features.

不同矿物的互层可以形成独特的地质特征。

6.The geologist studied the layers of rock, noting the interbedding of sandstone and shale.

地质学家研究了岩石层，注意到砂岩和页岩的互层。

7.In sedimentary formations, interbedding can indicate changes in depositional environments.

在沉积层中，互层可能表明沉积环境的变化。

8.Researchers found that the interbedding of limestone and clay affects the permeability of the aquifer.

研究人员发现石灰岩和粘土的互层影响了含水层的渗透性。

9.The interbedding of volcanic ash within the sedimentary rocks provided valuable information about past eruptions.

沉积岩中的火山灰互层提供了关于过去喷发的重要信息。

作文

In the realm of geology, the concept of interbedding plays a crucial role in understanding sedimentary rock formations. Interbedding refers to the layering of different types of sedimentary rocks, where distinct layers of one rock type alternate with layers of another. This phenomenon is often observed in environments where various sedimentary processes occur simultaneously, such as river deltas, lake beds, or marine settings. The study of interbedding not only helps geologists decipher the history of an area but also provides insights into past environmental conditions.For instance, when analyzing a core sample from a sedimentary basin, geologists may encounter sequences of sandstone, shale, and limestone that exhibit interbedding. Each layer represents a different depositional environment: sandstone might indicate a high-energy river environment, while shale could suggest a quieter, low-energy setting like a deep lake. By examining the characteristics of these layers, scientists can reconstruct the geological history of the region, including changes in climate, sea level, and tectonic activity.Furthermore, interbedding has significant implications for natural resource exploration, particularly in the fields of petroleum and groundwater. In many cases, reservoirs for oil and gas are found within specific rock types that are interbedded with less permeable layers. Understanding the patterns of interbedding allows geologists to better predict where these resources might be located and how they can be extracted efficiently.Moreover, interbedding can affect the mechanical properties of rocks, influencing their stability and behavior under stress. This is particularly important in civil engineering and construction, where the presence of interbedded layers can impact the design and safety of structures built on or within these geological formations. Engineers must consider the potential for differential settlement and other issues that may arise due to the varying characteristics of the interbedded rocks.The study of interbedding is not limited to sedimentary rocks alone; it can also be observed in volcanic and metamorphic contexts. For example, volcanic tuffs may exhibit interbedding of ash layers and lava flows, providing a record of eruptive events and the evolution of volcanic systems. Similarly, metamorphic rocks can show interbedding of different mineral compositions, reflecting the conditions under which they formed and the processes that have affected them over time.In conclusion, interbedding is a fundamental concept in geology that enhances our understanding of the Earth's history, resource distribution, and engineering challenges. By studying the various interbedded layers, geologists and engineers can glean valuable information about past environments, identify potential resources, and make informed decisions regarding construction and land use. As we continue to explore and learn about our planet, the significance of interbedding will undoubtedly remain a key focus in the field of earth sciences.

在地质学领域，interbedding的概念在理解沉积岩层中起着至关重要的作用。interbedding指的是不同类型的沉积岩的分层，其中一种岩石类型的不同层交替出现另一种岩石的层。这种现象通常在同时发生各种沉积过程的环境中观察到，例如河流三角洲、湖床或海洋环境。对interbedding的研究不仅帮助地质学家解读一个地区的历史，还提供了对过去环境条件的洞察。例如，在分析沉积盆地的岩心样本时，地质学家可能会遇到砂岩、页岩和石灰岩的序列，这些岩石表现出interbedding。每一层代表一个不同的沉积环境：砂岩可能表明高能量的河流环境，而页岩则可能暗示一个更安静、低能量的环境，如深湖。通过检查这些层的特征，科学家可以重建该地区的地质历史，包括气候、海平面和构造活动的变化。此外，interbedding对自然资源勘探有重要影响，特别是在石油和地下水领域。在许多情况下，油气的储层位于特定的岩石类型中，这些岩石与不太渗透的层交替出现。理解interbedding的模式使地质学家能够更好地预测这些资源可能的位置以及如何有效开采。此外，interbedding还会影响岩石的力学性质，影响它们在应力下的稳定性和行为。这在土木工程和建筑中尤为重要，因为存在交替层可能影响在这些地质形成物上或内部建造的结构的设计和安全性。工程师必须考虑由于交替岩石的不同特性而可能出现的差异沉降和其他问题。对interbedding的研究不仅限于沉积岩；它也可以在火山和变质背景中观察到。例如，火山凝灰岩可能表现出火山灰层和熔岩流的interbedding，提供了喷发事件和火山系统演变的记录。同样，变质岩可以显示出不同矿物成分的interbedding，反映出它们形成时的条件以及随着时间推移影响它们的过程。总之，interbedding是地质学中的一个基本概念，增强了我们对地球历史、资源分布和工程挑战的理解。通过研究各种交替层，地质学家和工程师可以获得关于过去环境的宝贵信息，识别潜在资源，并就建设和土地利用做出明智的决定。随着我们继续探索和了解我们的星球，interbedding的重要性无疑将继续成为地球科学领域的一个关键焦点。