basculating fault

简明释义

1. 走向移动断层; 2. 扭断层; 3. 挫断层; 4. 翘断层;

英英释义

A basculating fault refers to a type of geological fault that involves the tilting or rotation of rock layers, often resulting in changes in the orientation of strata.

基于倾斜的断层是指一种地质断层,涉及岩层的倾斜或旋转,通常导致地层方向的变化。

例句

1.We need to monitor for any signs of a basculating fault during the testing phase.

在测试阶段,我们需要监控任何倾斜故障的迹象。

2.The technician explained how a basculating fault can lead to system instability.

技术人员解释了倾斜故障如何导致系统不稳定。

3.After troubleshooting, we found that the basculating fault was due to a loose connection.

经过故障排除,我们发现倾斜故障是由于连接松动引起的。

4.The software update aims to fix the basculating fault reported by users.

软件更新旨在修复用户报告的倾斜故障

5.The engineer identified a basculating fault in the circuit that caused intermittent failures.

工程师在电路中识别出一个倾斜故障,导致间歇性故障。

作文

In the realm of geophysics, understanding various types of faults is crucial for both academic research and practical applications, particularly in the field of earthquake engineering. One such type of fault that has garnered attention is the basculating fault. The term ‘basculating fault’ refers to a specific kind of geological fault characterized by a rotational movement of the fault blocks. This movement can lead to significant geological formations and is often associated with tectonic activity. The concept of a basculating fault can be better understood by examining its mechanics and implications on the Earth's crust.To begin with, the mechanics of a basculating fault involve the tilting or rotating of rock masses along the fault line. This rotation can occur due to various geological processes, including tectonic plate movements, volcanic activity, or other stressors acting upon the Earth’s crust. As these forces interact, they can create a scenario where one block of rock rotates relative to another, resulting in the characteristic movement of a basculating fault. Understanding this mechanism is essential for predicting potential seismic activity in regions where such faults are present.The implications of a basculating fault extend beyond mere geological interest; they have real-world consequences, particularly in areas prone to earthquakes. For instance, regions that experience frequent seismic activity may have underlying basculating faults that contribute to the intensity and frequency of earthquakes. By studying these faults, scientists can better assess the risks associated with living in or near such areas. This knowledge is vital for urban planning, construction practices, and disaster preparedness initiatives.Moreover, the study of basculating faults also plays a role in understanding the broader context of tectonic movements. These faults can often be indicators of larger geological processes at play, such as continental drift or the formation of mountain ranges. By analyzing the characteristics and behaviors of basculating faults, geologists can gain insights into the historical movements of tectonic plates and the evolution of the Earth’s surface over millions of years.In conclusion, the significance of the basculating fault in geological studies cannot be overstated. Its unique characteristics and the mechanisms behind its movement provide valuable information for understanding the dynamics of the Earth’s crust. Furthermore, the practical implications of studying such faults are critical for ensuring safety and preparedness in earthquake-prone regions. As research continues to evolve, the insights gained from basculating faults will undoubtedly contribute to our overall understanding of geological processes and enhance our ability to mitigate the risks associated with seismic activities.

在地球物理学领域,理解各种类型的断层对于学术研究和实际应用尤其重要,特别是在地震工程领域。其中一个引起关注的断层类型是基轴故障。术语‘基轴故障’指的是一种特定类型的地质断层,其特征是断层块的旋转运动。这种运动可能导致显著的地质形成,并且通常与构造活动相关。通过研究其机制和对地壳的影响,可以更好地理解基轴故障的概念。首先,基轴故障的机制涉及沿断层线的岩石块的倾斜或旋转。这种旋转可能由于各种地质过程而发生,包括构造板块运动、火山活动或作用于地壳的其他压力源。当这些力量相互作用时,就会产生一种情形,其中一块岩石相对于另一块岩石旋转,从而导致基轴故障的特征性运动。理解这一机制对于预测这些断层存在的地区潜在的地震活动至关重要。基轴故障的影响超出了单纯的地质兴趣;它们在地震频发的地区具有现实世界的后果。例如,经历频繁地震活动的地区可能有潜在的基轴故障,这会影响地震的强度和频率。通过研究这些断层,科学家可以更好地评估生活在或靠近这些地区的风险。这些知识对于城市规划、建筑实践和灾难准备计划至关重要。此外,基轴故障的研究还在理解构造运动的更广泛背景中发挥着作用。这些断层常常是更大地质过程的指示器,例如大陆漂移或山脉的形成。通过分析基轴故障的特征和行为,地质学家可以深入了解构造板块的历史运动及地球表面数百万年来的演变。总之,基轴故障在地质研究中的重要性不容小觑。其独特的特征和运动背后的机制为理解地壳动态提供了宝贵的信息。此外,研究这些断层的实际意义对于确保地震频发地区的安全和准备至关重要。随着研究的不断发展,从基轴故障中获得的见解无疑将有助于我们对地质过程的整体理解,并增强我们减轻与地震活动相关风险的能力。