brachy synclinal fold

简明释义

短轴向斜褶皱;

英英释义

例句

1.The brachy synclinal fold 短轴向下褶皱 observed in this area is a result of compressive forces acting on the crust.

在该地区观察到的brachy synclinal fold 短轴向下褶皱是地壳上作用的压缩力的结果。

2.The geologist explained that the rock layers were shaped into a brachy synclinal fold 短轴向下褶皱, indicating a recent tectonic event.

地质学家解释说，岩层形成了一个brachy synclinal fold 短轴向下褶皱，这表明最近发生了构造事件。

3.In our research, we focused on the formation processes of the brachy synclinal fold 短轴向下褶皱 and its implications for resource distribution.

在我们的研究中，我们专注于brachy synclinal fold 短轴向下褶皱的形成过程及其对资源分布的影响。

4.During the field study, we observed a prominent brachy synclinal fold 短轴向下褶皱 that altered the local landscape significantly.

在实地研究中，我们观察到一个显著的brachy synclinal fold 短轴向下褶皱，它显著改变了当地的地形。

5.The brachy synclinal fold 短轴向下褶皱 was crucial for understanding the geological history of the region.

这个brachy synclinal fold 短轴向下褶皱 对于理解该地区的地质历史至关重要。

作文

In the study of geology, understanding various types of folds is crucial for interpreting the Earth's structure and the processes that shape it. One such fold is the brachy synclinal fold, which plays a significant role in the formation of landscapes and geological features. A brachy synclinal fold is characterized by its short wavelength and gentle slopes, creating a trough-like structure where the youngest rocks are found at the center, flanked by older rocks on either side. This type of fold is typically formed under compressional forces that act over a relatively short distance, leading to the bending and warping of rock layers. The formation of a brachy synclinal fold often occurs in regions where tectonic plates collide or converge. As these plates push against each other, the resulting stress can cause the rock layers to buckle and fold. Unlike other folds, such as anticlines, which arch upwards, a brachy synclinal fold dips downwards, creating a concave shape. This structural feature is essential for geologists to identify because it helps in predicting the location of natural resources, such as oil and gas deposits, which are often trapped within these folds. Moreover, the study of brachy synclinal folds provides valuable insights into the history of the Earth's crust. By analyzing the orientation and characteristics of these folds, geologists can reconstruct past geological events and understand the forces that have shaped the planet over millions of years. For instance, the presence of a brachy synclinal fold in an area can indicate previous tectonic activity, which may have implications for earthquake risk assessment and land-use planning. In addition to their geological significance, brachy synclinal folds also influence the landscape and ecology of an area. The trough-like shape created by these folds can affect drainage patterns, soil distribution, and vegetation growth. Areas surrounding a brachy synclinal fold may experience different microclimates due to variations in elevation and exposure to sunlight. This can lead to unique ecosystems that thrive in specific conditions, making these geological formations not only fascinating from a scientific perspective but also important for biodiversity conservation. In conclusion, the brachy synclinal fold is a fundamental concept in geology that exemplifies the dynamic nature of the Earth's crust. Its unique characteristics and formation processes provide essential information for understanding geological history, resource distribution, and ecological diversity. By studying brachy synclinal folds, geologists can gain a deeper appreciation for the complexities of our planet and the forces that continue to shape it today.

在地质学研究中，理解各种类型的褶皱对于解释地球的结构和形成地球的过程至关重要。其中一种褶皱是短波同步褶皱，它在地貌和地质特征的形成中发挥着重要作用。短波同步褶皱的特点是其短波长和温和的坡度，形成一个类似于槽的结构，最年轻的岩石位于中心，两侧夹着较老的岩石。这种类型的褶皱通常是在相对较短的距离内受到压缩力的作用下形成的，导致岩层的弯曲和变形。短波同步褶皱的形成通常发生在构造板块碰撞或汇聚的区域。当这些板块相互推挤时，产生的压力会导致岩层的弯曲和折叠。与其他褶皱（如拱状褶皱）不同，短波同步褶皱是向下倾斜的，形成凹形结构。这个结构特征对于地质学家识别非常重要，因为它有助于预测天然资源的位置，例如石油和天然气储藏，这些资源通常被困在这些褶皱中。此外，短波同步褶皱的研究提供了对地球地壳历史的宝贵见解。通过分析这些褶皱的方向和特征，地质学家可以重建过去的地质事件，并了解塑造地球的力量。例如，某个地区存在短波同步褶皱可能表明以前的构造活动，这可能对地震风险评估和土地利用规划具有重要意义。除了地质学的重要性，短波同步褶皱还影响着一个地区的地貌和生态。由于这些褶皱形成的槽状形状可能影响排水模式、土壤分布和植被生长。围绕短波同步褶皱的地区可能由于海拔和日照暴露的变化而经历不同的微气候。这可能导致在特定条件下繁荣的独特生态系统，使这些地质结构不仅从科学角度令人着迷，而且在生物多样性保护中也具有重要意义。总之，短波同步褶皱是地质学中的一个基本概念，体现了地球地壳的动态性质。它的独特特征和形成过程为理解地质历史、资源分布和生态多样性提供了重要信息。通过研究短波同步褶皱，地质学家能够更深入地理解我们星球的复杂性以及继续塑造它的力量。