anisometric crustal

简明释义

非等轴晶伐;

英英释义

Anisometric crustal refers to a type of geological crust characterized by varying dimensions and properties in different directions, indicating that the physical properties are not uniform across the material.

各向异性地壳是指一种地质地壳,其特征是在不同方向上具有不同的尺寸和性质,表明该材料的物理性质在各个方向上并不均匀。

例句

1.Research into anisometric crustal 各向异性地壳 dynamics is crucial for understanding earthquake mechanisms.

各向异性地壳 动力学的研究对于理解地震机制至关重要。

2.The study of the Earth's structure reveals that the anisometric crustal 各向异性地壳 properties can affect seismic wave propagation.

对地球结构的研究表明,各向异性地壳 性质会影响地震波传播。

3.Geologists often use models of anisometric crustal 各向异性地壳 behavior to predict the movement of tectonic plates.

地质学家常常使用各向异性地壳 行为模型来预测构造板块的运动。

4.The anisometric crustal 各向异性地壳 characteristics in this region indicate a complex geological history.

该地区的各向异性地壳 特征表明其复杂的地质历史。

5.The anisometric crustal 各向异性地壳 model helps geophysicists to interpret gravity anomalies.

各向异性地壳 模型帮助地球物理学家解释重力异常。

作文

The Earth's crust is a complex and dynamic layer that plays a crucial role in the geological processes that shape our planet. One of the fascinating aspects of the crust is its physical properties, which can vary significantly across different regions. Among these properties, the term anisometric crustal refers to the varying dimensions and characteristics of crustal materials in different directions. This concept is essential for understanding how geological forces interact with the Earth's surface and contribute to phenomena such as earthquakes, mountain formation, and volcanic activity.In geology, the term 'anisotropic' describes materials whose properties differ based on direction. When applied to the crust, anisometric crustal implies that the crust does not have uniform thickness or composition throughout its expanse. For instance, areas with significant tectonic activity often exhibit a more complex structure compared to stable regions. This anisometry can be attributed to various factors, including the history of tectonic movements, the type of rocks present, and the influence of external forces like erosion and sedimentation.Understanding the anisometric crustal nature of the Earth’s surface is vital for several reasons. Firstly, it aids geologists in predicting seismic activities. Regions with an anisometric crustal structure may experience different stress distributions during tectonic shifts, leading to varied seismic responses. By studying these patterns, scientists can better assess the risks associated with earthquakes and develop more effective warning systems.Secondly, the anisometric crustal features of the Earth can impact natural resource distribution. Minerals, oil, and gas are often found in specific geological formations that result from the unique characteristics of the crust in those areas. For example, the presence of faults and fractures, which are influenced by the anisometric nature of the crust, can create reservoirs for hydrocarbons. Thus, understanding the anisometry of the crust is essential for resource exploration and management.Moreover, the anisometric crustal properties play a significant role in landscape evolution. The uneven distribution of crustal materials leads to varied topographies, influencing everything from river paths to mountain ranges. For instance, mountains formed through tectonic uplift are often found in regions where the crust exhibits significant anisometry due to intense compressional forces. This results in dramatic landscapes that are both beautiful and scientifically intriguing.In conclusion, the concept of anisometric crustal is integral to our understanding of the Earth's geology. It highlights the complexity of the crust and its implications for seismic activity, resource distribution, and landscape formation. As we continue to study the Earth's crust, embracing the notion of anisometry will enable us to unlock further secrets of our planet's past, present, and future. By appreciating the intricate details of the anisometric crustal structure, we can enhance our knowledge of geological processes and their impact on human life and the environment.

地壳是一个复杂而动态的层次,在塑造我们星球的地质过程中发挥着至关重要的作用。地壳的一个迷人方面是其物理特性,这些特性在不同区域可能会显著变化。在这些特性中,术语各向异性地壳指的是地壳材料在不同方向上的尺寸和特征的变化。这个概念对于理解地质力量如何与地球表面相互作用并促成地震、山脉形成和火山活动等现象至关重要。在地质学中,“各向异性”一词描述的是材料的属性根据方向而异。当应用于地壳时,各向异性地壳意味着地壳在其广阔范围内并不具有均匀的厚度或成分。例如,具有显著构造活动的地区通常表现出比稳定区域更复杂的结构。这种各向异性可以归因于多种因素,包括构造运动的历史、存在的岩石类型以及侵蚀和沉积等外部力量的影响。理解地球的各向异性地壳特性至关重要,原因有几个。首先,它帮助地质学家预测地震活动。具有各向异性地壳结构的地区在构造变动期间可能经历不同的应力分布,从而导致不同的地震反应。通过研究这些模式,科学家可以更好地评估与地震相关的风险,并制定更有效的预警系统。其次,各向异性地壳特征对自然资源的分布也有影响。矿物、石油和天然气通常存在于由于地壳在这些区域的独特特性而形成的特定地质构造中。例如,受地壳各向异性影响的断层和裂缝的存在,可能为碳氢化合物创造储层。因此,理解地壳的各向异性对于资源勘探和管理至关重要。此外,各向异性地壳的特性在景观演变中也发挥了重要作用。地壳材料的不均匀分布导致了多样化的地形,影响从河流路径到山脉的方方面面。例如,通过构造抬升形成的山脉通常位于地壳表现出显著各向异性的地区,这些地区由于强烈的压缩力而形成。这导致了既美丽又科学上引人入胜的戏剧性景观。总之,各向异性地壳的概念对于我们理解地球的地质学至关重要。它突显了地壳的复杂性及其对地震活动、资源分布和景观形成的影响。随着我们继续研究地球的地壳,接受各向异性的概念将使我们能够解锁更多关于我们星球过去、现在和未来的秘密。通过欣赏各向异性地壳结构的复杂细节,我们可以增强对地质过程及其对人类生活和环境影响的认识。

相关单词

crustal

crustal详解:怎么读、什么意思、用法