antithetic faulting

简明释义

1. 反向断层作用; 2. 对偶断层作用;

英英释义

例句

1.The formation of valleys in this area can be attributed to antithetic faulting, which is a process involving 反向断层 that creates distinct geological features.

该地区山谷的形成可归因于 antithetic faulting，这是一种涉及 反向断层 的过程，创造出独特的地质特征。

2.Researchers are currently investigating the implications of antithetic faulting on local earthquake patterns, specifically how 反向断层 might influence seismic activity.

研究人员目前正在调查 antithetic faulting 对地方地震模式的影响，特别是 反向断层 如何影响地震活动。

3.The geological survey revealed that the region was characterized by antithetic faulting, which refers to 反向断层 where the faults move in opposing directions.

地质调查显示，该地区的特征是 antithetic faulting，即 反向断层，其中断层朝相反方向移动。

4.In studying the tectonic activity, we observed signs of antithetic faulting that suggested significant stress within the Earth's crust, known as 反向断层.

在研究构造活动时，我们观察到 antithetic faulting 的迹象，这表明地壳内存在显著的应力，即 反向断层。

5.The presence of antithetic faulting in this mountainous region indicates a complex history of geological evolution, marked by 反向断层 events.

这个山区中存在的 antithetic faulting 表明了复杂的地质演化历史，以 反向断层 事件为标志。

作文

In the study of geology, understanding various faulting mechanisms is crucial for comprehending the dynamics of Earth's crust. One such mechanism is known as antithetic faulting, which refers to a type of faulting where the secondary faults form in a direction opposite to that of the primary fault. This phenomenon can be observed in various tectonic settings and plays a significant role in shaping the landscape and influencing seismic activity. Antithetic faulting often occurs in response to extensional forces, where the Earth's crust is being pulled apart. As the primary fault slips, it creates a zone of weakness, allowing for the development of secondary faults that accommodate the ongoing deformation. These secondary faults typically dip in the opposite direction to the primary fault, creating a complex network of fractures within the rock mass. The significance of antithetic faulting extends beyond mere geological curiosity; it has practical implications for understanding earthquake mechanics and predicting seismic hazards. In regions where antithetic faulting is prevalent, the risk of earthquakes may be heightened due to the interaction between the primary and secondary faults. Moreover, this type of faulting can influence the distribution of natural resources, such as oil and gas deposits, as the movement of these faults can create traps for hydrocarbons. Recognizing the patterns of antithetic faulting is essential for geologists and engineers alike, as it aids in the assessment of potential drilling sites and the evaluation of stability in construction projects. Furthermore, the study of antithetic faulting contributes to our understanding of tectonic processes at a broader scale. By analyzing the characteristics and behaviors of these faults, researchers can gain insights into the historical movements of tectonic plates and the evolution of the Earth's crust over geological time. This knowledge not only enriches our scientific comprehension but also informs strategies for mitigating the impacts of natural disasters. In conclusion, antithetic faulting is a vital concept in geology that encapsulates the complexity of Earth's tectonic processes. Its implications reach far beyond the academic realm, affecting everything from resource management to earthquake preparedness. As we continue to explore the intricacies of our planet's geology, understanding mechanisms like antithetic faulting will remain essential for both scientific advancement and practical applications.

在地质学研究中，理解各种断层机制对于理解地球地壳的动态至关重要。其中一种机制被称为反向断层，指的是二级断层形成的方向与主断层相反的一种断层类型。这种现象可以在各种构造环境中观察到，并在塑造地貌和影响地震活动方面发挥着重要作用。反向断层通常发生在伸展力的作用下，即地球的地壳被拉开。当主断层滑动时，会形成一个弱区，允许二级断层的发展，以适应持续的变形。这些二级断层通常以与主断层相反的方向倾斜，在岩石体内形成复杂的裂缝网络。反向断层的重要性不仅仅是地质学的好奇心；它对理解地震力学和预测地震危害具有实际意义。在反向断层盛行的地区，由于主断层和二级断层之间的相互作用，地震的风险可能会增加。此外，这种类型的断层可以影响自然资源的分布，例如石油和天然气储量，因为这些断层的运动可能会为碳氢化合物创造陷阱。认识反向断层的模式对地质学家和工程师来说至关重要，因为它有助于评估潜在的钻探地点和评估建筑项目的稳定性。此外，反向断层的研究有助于我们理解更大规模的构造过程。通过分析这些断层的特征和行为，研究人员可以深入了解构造板块的历史运动以及地球地壳在地质时间上的演变。这一知识不仅丰富了我们的科学理解，还为减轻自然灾害影响的策略提供了依据。总之，反向断层是地质学中的一个重要概念，概括了地球构造过程的复杂性。它的影响远远超出了学术领域，影响着从资源管理到地震准备的方方面面。随着我们继续探索地球地质的复杂性，理解像反向断层这样的机制将始终对科学进步和实际应用至关重要。