hypocentral
简明释义
英[/ˌhaɪpəʊˈsɛntrəl/]美[/ˌhaɪpoʊˈsɛntrəl/]
震源定位
英英释义
Relating to the hypocenter, which is the point on the Earth's surface directly above the focus of an earthquake. | 与震源直接上方的地球表面点相关,称为震中。 |
单词用法
震源坐标 | |
震源距离 | |
震源地震波 | |
计算震源位置 | |
确定震源深度 | |
报告震源震级 |
同义词
震源 | The earthquake's hypocenter was located deep beneath the surface. | 这次地震的震源位于地表下深处。 | |
焦点 | Seismologists measure the distance from the focus of the earthquake to assess its impact. | 地震学家测量震中与震源的距离以评估其影响。 |
反义词
例句
1.The events were relocated using standard computer codes for hypocentral locations.
用震源位置的标准计算机码重新定位地震事件。
2.The events were relocated using standard computer codes for hypocentral locations.
用震源位置的标准计算机码重新定位地震事件。
3.Seismologists use various tools to analyze the hypocentral depths of earthquakes.
地震学家使用各种工具来分析地震的震源深度。
4.The seismic waves originated from the hypocentral point of the fault line.
地震波源自断层线的震源点。
5.The earthquake's hypocentral location was determined to be 10 kilometers below the surface.
这次地震的震源位置被确定在地下10公里处。
6.Understanding the hypocentral parameters helps in predicting aftershocks.
理解震源参数有助于预测余震。
7.The hypocentral coordinates provided crucial information for disaster response teams.
提供的震源坐标对灾害响应团队至关重要。
作文
In the study of seismology, understanding the terms used to describe earthquakes is crucial for both scientists and the general public. One such term is hypocentral, which refers to the point within the Earth where an earthquake originates. This point is located directly beneath the surface location of the earthquake, known as the epicenter. The concept of hypocentral is essential for accurately assessing the impact and magnitude of seismic events. When an earthquake occurs, it generates seismic waves that travel through the Earth. These waves can be detected by seismographs, which record the intensity and duration of the shaking. The data collected from these instruments help scientists determine the location of the hypocentral point. By analyzing the time it takes for seismic waves to reach various monitoring stations, researchers can triangulate the exact depth and position of the earthquake's origin. The depth of the hypocentral point can vary significantly from one earthquake to another. Shallow earthquakes, which occur at depths less than 70 kilometers, tend to cause more damage because they are closer to the Earth's surface. In contrast, deep-focus earthquakes, which occur at depths greater than 300 kilometers, often have less surface impact. However, understanding the hypocentral depth is vital for predicting the potential damage and response needed in affected areas. The relationship between the hypocentral point and the epicenter is also important for emergency management and disaster preparedness. Knowing the exact location of the hypocentral point allows authorities to assess the risk to nearby communities and infrastructure. For instance, if a hypocentral point is located near a densely populated area, emergency services can mobilize resources more effectively and provide timely warnings to residents. Moreover, the study of hypocentral points has led to significant advancements in our understanding of tectonic plate movements and the geological processes that drive earthquakes. By mapping the locations of hypocentral points over time, scientists can identify patterns and trends in seismic activity. This information is invaluable for developing models that predict future earthquakes and improve building codes to withstand seismic forces. In conclusion, the term hypocentral plays a critical role in the field of seismology. It not only helps in understanding the mechanics of earthquakes but also aids in disaster preparedness and response efforts. As our knowledge of seismic activity continues to evolve, the importance of accurately identifying and analyzing hypocentral points will remain a priority for researchers and policymakers alike. With continued research and technological advancements, we can hope to mitigate the effects of earthquakes on our communities and enhance our resilience to these natural disasters.
在地震学的研究中,理解描述地震的术语对于科学家和公众来说都是至关重要的。其中一个术语是hypocentral,它指的是地震发生的点,这个点位于地球内部,直接位于地震的表面位置,即震中之下。hypocentral的概念对于准确评估地震事件的影响和强度至关重要。当地震发生时,它会产生通过地球传播的地震波。这些波可以被地震仪检测到,记录震动的强度和持续时间。从这些仪器收集的数据帮助科学家确定hypocentral点的位置。通过分析地震波到达各个监测站的时间,研究人员可以三角测量出地震的确切深度和位置。hypocentral点的深度在不同地震中可能有显著差异。浅层地震发生在70公里以下的深度,往往造成更大的损害,因为它们离地表更近。相比之下,深源地震发生在300公里以上的深度,通常对地表影响较小。然而,了解hypocentral深度对于预测潜在的损害和受影响地区所需的响应至关重要。hypocentral点与震中之间的关系对于应急管理和灾难准备也很重要。知道hypocentral点的确切位置使当局能够评估附近社区和基础设施的风险。例如,如果hypocentral点位于一个人口稠密的地区,应急服务可以更有效地调动资源,并向居民提供及时警告。此外,对hypocentral点的研究推动了我们对构造板块运动和驱动地震的地质过程的理解。通过绘制hypocentral点的位置图,科学家可以识别地震活动的模式和趋势。这些信息对于开发预测未来地震的模型以及改善建筑规范以承受地震力是非常宝贵的。总之,术语hypocentral在地震学领域中扮演着关键角色。它不仅有助于理解地震的机制,还有助于灾害准备和响应工作。随着我们对地震活动的知识不断发展,准确识别和分析hypocentral点的重要性将继续成为研究人员和政策制定者的优先事项。随着研究和技术的不断进步,我们可以希望减轻地震对我们社区的影响,并增强我们对这些自然灾害的韧性。