seismometry

简明释义

英[ˌsaɪzməˈmɛtri]美[ˌsaɪzməˈmɛtri]

n. 测震学；测地震术

英英释义

单词用法

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例句

1.Fifth, there appeared trend anomalies of seismometry results and other microscopic precursors, implying that middle-term risk of strong earthquake exists in the determined monitoring region.

五是测震和其它微观前兆趋势性异常出现，说明所圈定监视区的中期强震危险性存在。

2.Fifth, there appeared trend anomalies of seismometry results and other microscopic precursors, implying that middle-term risk of strong earthquake exists in the determined monitoring region.

五是测震和其它微观前兆趋势性异常出现，说明所圈定监视区的中期强震危险性存在。

3.Borehole strain observation has been admitted, following seismometry and GPS, a most important means to monitor real-time crustal deformation.

钻孔应变观测正在成为一种与测震和GPS相提并论的地壳形变观测。

4.In dissimilar areas the seismometry and precursory items that appear more frequently are different, which reveal the regional distinction.

不同的区域异常出现率高的测震和前兆测项不同，显示出区域差异。

5.By means of this ratio and T_1, T_2, determined by seismometry, the mid long-term forecasting of earthquakes can be done.

利用此比值常数以及由测震学指标所确定的T_1和求得的T_2可以进行确定性的中长期地震预报。

6.The study of earthquakes relies heavily on seismometry 地震测量法 to provide accurate data.

地震研究在很大程度上依赖于seismometry 地震测量法来提供准确的数据。

7.Advancements in seismometry 地震测量法 have improved our ability to predict seismic events.

在seismometry 地震测量法方面的进步提高了我们预测地震事件的能力。

8.Researchers use seismometry 地震测量法 to analyze the Earth's internal structure.

研究人员使用seismometry 地震测量法来分析地球的内部结构。

9.The installation of new seismometry 地震测量法 equipment has enhanced monitoring capabilities.

新安装的seismometry 地震测量法设备增强了监测能力。

10.In regions prone to earthquakes, seismometry 地震测量法 is essential for public safety.

在易发生地震的地区，seismometry 地震测量法对公众安全至关重要。

作文

Seismometry is the scientific study of seismic waves and their effects on the Earth. This field of study is crucial for understanding the dynamics of the Earth's interior and the processes that lead to earthquakes. The instruments used in this field, known as seismometers, are designed to detect and record the vibrations caused by seismic waves. These vibrations can originate from various sources, including tectonic plate movements, volcanic activity, and even human-induced events such as explosions. By analyzing the data collected through seismometry (地震测量), scientists can gain valuable insights into the structure of the Earth and the mechanisms that drive geological phenomena. One of the primary applications of seismometry (地震测量) is earthquake monitoring. In regions prone to seismic activity, networks of seismometers are deployed to provide real-time data on earthquakes. This information is vital for early warning systems that can alert populations before destructive shaking occurs. The ability to predict when and where an earthquake might strike can save lives and minimize property damage. Furthermore, the data collected through seismometry (地震测量) contributes to the development of building codes and construction practices that enhance the resilience of structures against seismic forces. In addition to its role in earthquake monitoring, seismometry (地震测量) also plays a significant part in the exploration of natural resources. For instance, oil and gas companies utilize seismic surveys to locate potential drilling sites. By sending sound waves into the ground and analyzing the reflected waves, geophysicists can create images of subsurface formations. This technique not only aids in resource extraction but also helps in assessing the environmental impact of such activities. Moreover, seismometry (地震测量) has applications beyond Earth. Scientists are increasingly interested in the seismic activity of other celestial bodies, such as the Moon and Mars. By studying seismic waves on these planets, researchers can learn about their internal structures and geological histories. This research expands our understanding of planetary formation and evolution, offering clues about the conditions that may support life elsewhere in the universe. The advancement of technology has significantly enhanced the capabilities of seismometry (地震测量). Modern seismometers are highly sensitive and can detect even the smallest vibrations. Additionally, the integration of digital technology and data analysis techniques has revolutionized how seismological data is processed and interpreted. With the rise of machine learning and artificial intelligence, researchers can now analyze vast amounts of seismic data more efficiently, leading to improved predictions and better understanding of seismic hazards. In conclusion, seismometry (地震测量) is a vital scientific discipline that provides essential insights into the Earth's processes and helps mitigate the risks associated with seismic activity. Its applications range from earthquake monitoring to resource exploration and planetary science. As technology continues to evolve, the field of seismometry (地震测量) will undoubtedly play an increasingly important role in enhancing our understanding of the Earth and the universe beyond it.