isoclinal

简明释义

英[ˌaɪsəʊˈklaɪnəl]美[ˌaɪsəˈklaɪnəl]

adj. 等倾的；等伏角的

英英释义

单词用法

同义词

反义词

例句

1.If both limbs of overturned fold have same dip Angle we call this special overturned fold isoclinal fold.

如果倒转褶皱构造的两翼倾角相等，则可称这种特殊类型的倒转褶皱为等斜褶皱。

2.If both limbs of overturned fold have same dip Angle we call this special overturned fold isoclinal fold.

如果倒转褶皱构造的两翼倾角相等，则可称这种特殊类型的倒转褶皱为等斜褶皱。

3.The geological map shows several isoclinal 等斜的 folds that indicate significant tectonic activity in the region.

地质图显示出几个isoclinal 等斜的 褶皱，表明该地区发生了显著的构造活动。

4.During the field study, we identified an isoclinal 等斜的 fold that was crucial for understanding the area's geological history.

在实地研究中，我们识别出一个isoclinal 等斜的 褶皱，这对理解该地区的地质历史至关重要。

5.Geologists often study isoclinal 等斜的 folds to predict natural resource locations.

地质学家经常研究isoclinal 等斜的 褶皱以预测自然资源的位置。

6.The isoclinal 等斜的 nature of the rock layers suggests they were formed under uniform pressure conditions.

岩层的isoclinal 等斜的 特性表明它们是在均匀压力条件下形成的。

7.The presence of isoclinal 等斜的 structures can complicate the extraction of minerals.

存在isoclinal 等斜的 结构可能会使矿物的提取变得复杂。

作文

In the field of geology, the term isoclinal refers to a specific type of fold in rock layers where the limbs of the fold are inclined at the same angle. This phenomenon is crucial for understanding the structural characteristics of geological formations. When geologists study rock formations, they often encounter various types of folds, and recognizing the isoclinal folds can provide significant insights into the history of the Earth's crust. Isoclinal folds typically indicate that the rocks have undergone intense pressure and deformation, which can be associated with tectonic activities such as mountain-building processes. These folds can be observed in many regions around the world, often serving as key indicators of the geological past. For instance, in areas where isoclinal folds are prevalent, it may suggest that the region has experienced significant compressional forces. This understanding is vital for geologists when mapping out the geological history of an area, as well as for predicting potential natural resources that may be found within these folded structures.Moreover, the study of isoclinal folds extends beyond mere academic interest; it has practical implications in fields such as civil engineering and environmental science. Understanding the orientation and stability of these folds can influence construction projects, especially in hilly or mountainous terrains. Engineers must consider the geological features when designing buildings, roads, and other infrastructures to ensure safety and longevity. Furthermore, isoclinal folds can also impact the flow of groundwater and oil reservoirs, making their study essential for resource management.The identification of isoclinal folds can often be done through field studies and geological mapping. Geologists look for specific indicators such as the symmetry of the folds and the angles at which the layers are inclined. Advanced techniques like seismic surveys and satellite imaging are increasingly being used to analyze these geological structures from a broader perspective. As technology advances, the ability to study isoclinal folds and their implications will continue to improve, allowing for more accurate predictions and assessments of geological phenomena.In conclusion, the concept of isoclinal folds is fundamental in geology, providing insight into the dynamic processes that shape our planet. By studying these folds, geologists can unravel the complex history of the Earth's crust, inform construction practices, and manage natural resources more effectively. The ongoing research in this area is not only academically enriching but also essential for practical applications in various industries. As we continue to explore the intricacies of geological formations, the significance of isoclinal folds will remain a pivotal topic in understanding the Earth's structure and its resources.

在地质学领域，术语isoclinal指的是一种特定类型的岩层褶皱，其中褶皱的两侧以相同的角度倾斜。这种现象对于理解地质构造的特征至关重要。当地质学家研究岩石形成时，他们经常会遇到各种类型的褶皱，而识别isoclinal褶皱可以为了解地球地壳的历史提供重要见解。Isoclinal褶皱通常表明岩石经历了强烈的压力和变形，这可能与构造活动如造山过程相关联。这些褶皱可以在世界许多地区观察到，通常作为地质过去的关键指标。例如，在isoclinal褶皱盛行的地区，可能表明该区域经历了显著的压缩力。这种理解对于地质学家绘制一个地区的地质历史至关重要，同时也有助于预测这些折叠结构中可能发现的自然资源。此外，isoclinal褶皱的研究超出了单纯的学术兴趣；它在土木工程和环境科学等领域也具有实际意义。了解这些褶皱的方向和稳定性可以影响建设项目，特别是在丘陵或山区地形中。工程师在设计建筑、道路和其他基础设施时，必须考虑地质特征，以确保安全和持久性。此外，isoclinal褶皱还会影响地下水流动和油气储藏，使其研究对资源管理至关重要。Isoclinal褶皱的识别通常可以通过实地研究和地质测绘来完成。地质学家寻找特定的指标，如褶皱的对称性和岩层倾斜的角度。先进的技术如地震勘测和卫星成像正越来越多地被用于从更广阔的视角分析这些地质结构。随着技术的进步，研究isoclinal褶皱及其影响的能力将继续提高，从而使对地质现象的预测和评估更加准确。总之，isoclinal褶皱的概念在地质学中是基础性的，为揭示塑造我们星球的动态过程提供了见解。通过研究这些褶皱，地质学家能够解开地球地壳复杂的历史，更有效地为建筑实践提供信息，并管理自然资源。该领域的持续研究不仅在学术上是丰富的，而且在各个行业的实际应用中也是必不可少的。随着我们继续探索地质形成的复杂性，isoclinal褶皱的重要性将始终是理解地球结构及其资源的关键主题。