geodynamical

简明释义

英[ˌdʒiːəʊdaɪˈnæmɪkəl]美[ˌdʒiːoʊdaɪˈnæmɪkəl]

adj. 地球动力学的

英英释义

单词用法

同义词

反义词

例句

1.Temperature measurements and its long-period observation will provide reliable basic data for geothermal and geodynamical study of the ultra-high pressure metamorphic belt.

大陆科学钻探温度测量，为今后进一步研究超高压变质带深部地热场及其地球动力学含义提供了可靠的基础数据。

2.Temperature measurements and its long-period observation will provide reliable basic data for geothermal and geodynamical study of the ultra-high pressure metamorphic belt.

大陆科学钻探温度测量，为今后进一步研究超高压变质带深部地热场及其地球动力学含义提供了可靠的基础数据。

3.The REE geochemical research has provided the important evidence for the mechanism of the Premian post-collision stage and the geodynamical evolution process.

稀土元素地球化学研究为新疆准噶尔地区二叠纪后碰撞阶段的岩浆作用机理及地球动力学演化过程提供了重要证据。

4.Seismological and geodynamical evidences supported whole mantle convection model, while geochemical ones supported layered convection model.

地震学、地球动力学研究倾向于全地幔对流模型；地球化学研究则支持分层地幔对流。

5.The study of geodynamical 地球动力学的 processes is essential for understanding plate tectonics.

研究地球动力学的过程对于理解板块构造至关重要。

6.Researchers are using geodynamical 地球动力学的 models to predict volcanic eruptions.

研究人员正在使用地球动力学的模型来预测火山喷发。

7.The geodynamical 地球动力学的 behavior of the Earth's mantle influences seismic activity.

地球地幔的地球动力学的行为影响地震活动。

8.Understanding geodynamical 地球动力学的 forces can help in assessing natural disaster risks.

理解地球动力学的力量有助于评估自然灾害风险。

9.Geologists often rely on geodynamical 地球动力学的 simulations to explore Earth's internal processes.

地质学家通常依赖地球动力学的模拟来探索地球内部过程。

作文

The Earth is a dynamic system, constantly undergoing changes that affect its structure and surface. One of the key areas of study in understanding these changes is the field of geodynamical (地球动力学) processes. Geodynamical studies focus on the physical processes that drive the movement of the Earth's crust, the formation of mountains, the occurrence of earthquakes, and the dynamics of plate tectonics. These processes are essential for comprehending not only the Earth's past but also its future evolution. One of the most significant aspects of geodynamical (地球动力学) research is the investigation of plate tectonics. The Earth's lithosphere is divided into several large and small plates that float on the semi-fluid asthenosphere beneath them. The interactions between these tectonic plates can lead to various geological phenomena, such as volcanic eruptions and seismic activity. Understanding these interactions helps scientists predict natural disasters and assess their potential impact on human life and infrastructure. Additionally, geodynamical (地球动力学) processes are not limited to just plate movements. They also encompass the study of mantle convection, which is the slow movement of the Earth's mantle caused by heat from the core. This convection drives the movement of tectonic plates and is responsible for many geological features we observe today. By employing advanced models and simulations, researchers can gain insights into how these processes have shaped the planet over millions of years. Another crucial area of geodynamical (地球动力学) study is the analysis of stress and strain within the Earth's crust. As tectonic plates interact, they accumulate stress until it is released in the form of an earthquake. By studying the patterns of stress accumulation and release, scientists can better understand earthquake mechanics and potentially improve early warning systems. This knowledge is vital for regions prone to seismic activity, where preparedness can save lives and reduce economic losses. Moreover, geodynamical (地球动力学) research also has implications for understanding climate change. The movement of tectonic plates can influence ocean currents and atmospheric conditions, which in turn affect global climate patterns. For instance, the uplift of mountain ranges can alter wind patterns and precipitation, while the shifting of continents can impact ocean circulation. By integrating geodynamical (地球动力学) data with climate models, scientists can develop more accurate predictions of how our planet's climate may change in response to both natural and anthropogenic influences. In conclusion, the study of geodynamical (地球动力学) processes is fundamental to our understanding of the Earth's behavior and its ongoing evolution. From plate tectonics and mantle convection to stress accumulation and climate interactions, the insights gained from this field are invaluable. As we continue to face challenges such as natural disasters and climate change, the importance of geodynamical (地球动力学) research cannot be overstated. It provides the scientific foundation necessary for informed decision-making and effective risk management, ensuring that we are better prepared for the future.

地球是一个动态系统，持续经历影响其结构和表面的变化。理解这些变化的关键领域之一是地球动力学（geodynamical）过程的研究。地球动力学（geodynamical）研究集中于驱动地壳运动、山脉形成、地震发生和板块构造动态的物理过程。这些过程对于理解地球的过去以及未来的演变至关重要。 地球动力学（geodynamical）研究中最重要的方面之一是对板块构造的调查。地球的岩石圈被分为几个大大小小的板块，这些板块漂浮在下面半流体的软流圈上。这些构造板块之间的相互作用可以导致各种地质现象，例如火山喷发和地震活动。理解这些相互作用有助于科学家预测自然灾害并评估其对人类生活和基础设施的潜在影响。 此外，地球动力学（geodynamical）过程不仅限于板块运动。它们还包括对地幔对流的研究，这是由于地核热量引起的地球地幔的缓慢运动。这种对流驱动着构造板块的运动，并且负责我们今天观察到的许多地质特征。通过采用先进的模型和模拟，研究人员可以深入了解这些过程如何在数百万年中塑造了地球。 另一个重要的地球动力学（geodynamical）研究领域是对地壳内应力和应变的分析。当构造板块相互作用时，它们会积累应力，直到以地震的形式释放出来。通过研究应力积累和释放的模式，科学家可以更好地理解地震机制，并可能改善早期预警系统。这一知识对于地震活动频繁的地区至关重要，在这些地区，准备工作可以拯救生命并减少经济损失。 此外，地球动力学（geodynamical）研究还对理解气候变化具有重要意义。构造板块的运动可以影响海洋洋流和大气条件，从而影响全球气候模式。例如，山脉的隆起可以改变风的模式和降水，而大陆的移动可以影响海洋环流。通过将地球动力学（geodynamical）数据与气候模型结合，科学家可以更准确地预测我们星球的气候如何因自然和人为影响而变化。 总之，地球动力学（geodynamical）过程的研究是我们理解地球行为及其持续演变的基础。从板块构造和地幔对流到应力积累和气候相互作用，这一领域所获得的见解都是无价的。随着我们继续面临自然灾害和气候变化等挑战，地球动力学（geodynamical）研究的重要性不容小觑。它为明智决策和有效风险管理提供了必要的科学基础，确保我们为未来做好更好的准备。