monocline

简明释义

[ˈmɒnəʊˌklaɪn][ˈmɑːnəˌklaɪn]

n. 单斜层;单斜褶皱

英英释义

A monocline is a geological formation in which rock layers are folded or tilted in one direction, creating a step-like structure.

单斜是指一种地质构造,其中岩层在一个方向上折叠或倾斜,形成台阶状结构。

单词用法

monocline structure

单斜结构

monocline formation

单斜形成

a monocline fold

一个单斜褶皱

the monocline theory

单斜理论

同义词

fold

褶皱

The geological structure features a prominent fold that indicates significant tectonic activity.

该地质结构的特征是一个显著的褶皱,表明了显著的构造活动。

tilt

倾斜

The rock layers exhibit a noticeable tilt towards the east, suggesting a monocline formation.

岩层向东显著倾斜,暗示了单斜的形成。

反义词

fold

褶皱

The geological structure of the region is characterized by a complex fold system.

该地区的地质结构以复杂的褶皱系统为特征。

unconformity

不整合面

An unconformity indicates a gap in the geological record.

不整合面表明地质记录中的一个间隙。

例句

1.The effect of electrocast zirconia and monocline zirconia and two types of binders(anhydrous and un-hydroxyl resin and liquid paraffin)on the sintering of fired magnesia-calcia brick are investigated.

研究了电熔氧化锆、单斜氧化锆和两种结合剂(无水无羟基树脂和液体石蜡)对烧成镁钙砖烧结性能的影响。

2.Dexing Basin is generally a monocline downfaulted one with north-dipping rock format ion.

德兴盆地大体上是一个岩层向北倾斜的单斜式断陷盆地。

3.The eastern part is multi-stages fan delta deposit system witch is controlled by the monocline and step-fault zone and another parts in the area grow alluvial fan system.

东部为单斜、顺向断阶带构造背景控制下的多期次的扇三角洲沉积体系,部分地方发育冲积扇体系。

4.Characteristic: Blue green monocline crystallization, dissolve it in water, glycerin, does not allow it in the ethanol, There is corrosive, deliquescence in weathered.

性状:兰绿色单斜结晶,容于水、甘油,不容于乙醇,有腐蚀性,潮解风化。

5.The effect of electrocast zirconia and monocline zirconia and two types of binders(anhydrous and un-hydroxyl resin and liquid paraffin)on the sintering of fired magnesia-calcia brick are investigated.

研究了电熔氧化锆、单斜氧化锆和两种结合剂(无水无羟基树脂和液体石蜡)对烧成镁钙砖烧结性能的影响。

6.The Hengdan turbidite sequence is composed of very thick, normal turbidity current deposits. It is marked by a monocline dipping south or southeast.

南秦岭横丹浊积岩系是一套巨厚的浊流沉积,以向南或南东倾的单斜构造产出。

7.The deeper structure appears to be a gently warped monocline.

较深构造仿佛是轻度翘曲的单斜。

8.In addition to these two types of folds, however, we must mention another one, which is not easily classifiable as either anticline or syncline and is referred to as a monocline.

然而,除了上述两种褶皱外,我们还必须提到另外一种,这种褶皱不易归类为背斜或向斜,而被称为单斜褶皱。

9.Studying the monocline helps geologists understand the tectonic forces at play.

研究单斜层有助于地质学家理解作用的构造力量。

10.In the canyon, we could see the layers of rock bending into a monocline.

在峡谷中,我们可以看到岩层弯曲成一个单斜层

11.The monocline formed as a result of compressional stress in the Earth's crust.

这个单斜层是由于地壳中的压缩应力形成的。

12.The geological survey revealed that the region was characterized by a prominent monocline.

地质调查显示该地区的特征是一个显著的单斜层

13.The monocline is an important feature for understanding regional geology.

这个单斜层是理解区域地质的重要特征。

作文

In the study of geology, understanding various structural features of the Earth's crust is crucial for comprehending its dynamic nature. One such feature is a monocline, which is a geological formation characterized by a step-like fold in rock layers. This formation occurs when there is a significant shift in the orientation of the rock strata, typically due to tectonic forces. In simpler terms, a monocline can be visualized as a staircase where the steps represent different layers of rock that have been pushed up or tilted at an angle. The study of monoclines provides valuable insights into the geological history of an area, including past tectonic activity and the processes that shaped the landscape we see today.The formation of a monocline often results from the bending of rock layers due to faulting or warping. When tectonic plates move, they exert pressure on the Earth's crust, causing it to deform. This deformation can lead to the creation of a monocline, which may extend for miles and can vary significantly in height and steepness. For geologists, identifying a monocline is essential because it can indicate the presence of underlying geological structures, such as faults or folds, that are not immediately visible on the surface.Moreover, monoclines can influence local ecosystems and water drainage patterns. The slope created by a monocline can affect how water flows across the landscape, leading to the formation of rivers, lakes, and wetlands in certain areas while leaving others dry. This aspect of monoclines highlights the interconnectedness of geological formations and ecological systems, demonstrating that changes in the Earth’s structure can have far-reaching effects on the environment.In addition to their ecological significance, monoclines are also of great interest in the field of natural resources. Many mineral deposits, including coal and oil, are found in association with these geological structures. Understanding the location and formation of monoclines can aid in the exploration and extraction of these valuable resources. Therefore, geologists and resource companies often conduct detailed studies of monoclines to identify potential sites for mining or drilling.The study of monoclines also plays a vital role in assessing geological hazards. Regions with pronounced monoclines may be more susceptible to landslides or other forms of erosion, especially during heavy rainfall. By understanding the characteristics and distribution of monoclines, scientists can better predict and mitigate the risks associated with these natural disasters, ultimately helping to protect communities and infrastructure.In conclusion, the concept of a monocline is fundamental to our understanding of geological processes and their implications for the environment and human activity. From influencing local ecosystems to guiding resource exploration and hazard assessment, monoclines are a key component of the Earth’s complex geological framework. As we continue to explore and study these fascinating formations, we gain deeper insights into the dynamic processes that shape our planet and the resources it provides. Thus, the significance of monoclines extends far beyond their geological definition; they are integral to understanding the Earth's past, present, and future.

在地质学的研究中,理解地壳的各种结构特征对于理解其动态特性至关重要。一个这样的特征是单斜层,它是一种以阶梯状褶皱为特征的岩石层地质构造。这种构造发生在岩石层的方向发生显著变化时,通常是由于构造力的作用。简单来说,单斜层可以被视为一个楼梯,其中的台阶代表不同的岩石层,这些岩石层被推起或倾斜成一定角度。对单斜层的研究为我们提供了有关一个地区地质历史的宝贵见解,包括过去的构造活动和塑造我们今天所见景观的过程。单斜层的形成通常是由于断层或翘曲导致的岩层弯曲。当构造板块移动时,它们对地壳施加压力,导致其变形。这种变形可能导致单斜层的形成,单斜层可能延伸数英里,并且在高度和陡峭程度上可能有显著变化。对于地质学家来说,识别单斜层至关重要,因为它可以指示地下地质结构的存在,如在地表上不立即可见的断层或褶皱。此外,单斜层还可以影响当地生态系统和水流模式。单斜层所造成的坡度可以影响水在景观中的流动方式,导致某些地区形成河流、湖泊和湿地,而其他地区则干旱。单斜层的这一方面突出了地质构造与生态系统之间的相互联系,表明地球结构的变化可以对环境产生深远的影响。除了生态意义外,单斜层在自然资源领域也引起了极大的兴趣。许多矿藏,包括煤和石油,与这些地质构造相关联。了解单斜层的位置和形成可以帮助探索和开采这些宝贵资源。因此,地质学家和资源公司通常会对单斜层进行详细研究,以识别潜在的采矿或钻探地点。单斜层的研究在评估地质灾害方面也发挥着重要作用。具有明显单斜层的地区可能更容易发生滑坡或其他形式的侵蚀,尤其是在强降雨期间。通过了解单斜层的特征和分布,科学家可以更好地预测和减轻与这些自然灾害相关的风险,最终帮助保护社区和基础设施。总之,单斜层的概念对于我们理解地质过程及其对环境和人类活动的影响至关重要。从影响当地生态系统到指导资源探索和危险评估,单斜层是地球复杂地质框架的关键组成部分。随着我们继续探索和研究这些迷人的构造,我们对塑造我们星球的动态过程有了更深入的认识,以及它所提供的资源。因此,单斜层的重要性远远超出了其地质定义;它们是理解地球过去、现在和未来的不可或缺的一部分。