neotectonic age

简明释义

新构造年龄;

英英释义

例句

1.The landscape has been dramatically altered due to processes occurring during the neotectonic age 新构造时代.

由于在新构造时代 neotectonic age发生的过程，地形发生了剧烈变化。

2.The study of the region's geology revealed significant changes during the neotectonic age 新构造时代.

该地区的地质研究揭示了在新构造时代 neotectonic age期间发生的重要变化。

3.Dating sediments from the neotectonic age 新构造时代 helps us understand past climate conditions.

对来自新构造时代 neotectonic age的沉积物进行年代测定有助于我们理解过去的气候条件。

4.Understanding the neotectonic age 新构造时代 is crucial for predicting seismic activity in the area.

了解新构造时代 neotectonic age对于预测该地区的地震活动至关重要。

5.Geologists have discovered fault lines that were formed in the neotectonic age 新构造时代.

地质学家发现了一些在新构造时代 neotectonic age形成的断层线。

作文

The concept of neotectonic age refers to the period in geological time when the Earth's crust has been significantly influenced by tectonic processes, particularly since the late Cenozoic era. Understanding the neotectonic age is crucial for geologists and earth scientists as it provides insights into the dynamic nature of our planet's surface and helps in predicting geological hazards such as earthquakes and volcanic eruptions. The term 'neotectonics' itself is derived from the Greek word 'neo,' meaning 'new,' and 'tectonics,' which pertains to the structure and movement of the Earth's crust. Thus, neotectonic age encompasses the recent geological history where active tectonic movements have shaped landscapes and influenced sedimentation patterns.During the neotectonic age, various regions around the world have experienced significant geological changes due to the movement of tectonic plates. For instance, the Himalayas continue to rise as the Indian plate collides with the Eurasian plate, a process that has been ongoing since the late Mesozoic but has accelerated during the neotectonic age. This collision not only creates majestic mountain ranges but also triggers seismic activities that can lead to devastating earthquakes. Therefore, studying the neotectonic age allows scientists to assess risks in regions prone to such natural disasters.Moreover, the neotectonic age is characterized by the formation of various geological features, including faults, folds, and rift valleys. These structures are the result of stress and strain accumulated in the Earth's crust due to tectonic forces. For example, the San Andreas Fault in California is a well-known transform fault that exemplifies the active tectonic processes occurring in the region. By analyzing the characteristics of faults formed during the neotectonic age, researchers can better understand the mechanics of earthquakes and develop more effective mitigation strategies.In addition to its significance in understanding geological hazards, the neotectonic age also plays a vital role in resource management. Regions that are still tectonically active often have abundant natural resources such as minerals, oil, and gas. The movement of tectonic plates can lead to the concentration of these resources, making them economically valuable. Therefore, knowledge of the neotectonic age can aid in exploration and sustainable management of these resources, ensuring that they are utilized responsibly without causing harm to the environment.Furthermore, the study of the neotectonic age extends beyond Earth sciences; it intersects with fields such as archaeology and anthropology. Many ancient civilizations developed in areas that are now recognized as tectonically active zones. Understanding the geological history of these regions can provide context for human settlement patterns, agricultural practices, and even architectural styles. For instance, the ruins of ancient cities in earthquake-prone areas offer valuable lessons about resilience and adaptation to natural disasters, which are still relevant today.In conclusion, the neotectonic age is a significant period in geological history that reflects the ongoing processes shaping our planet. Its study is essential for understanding natural hazards, managing resources, and appreciating the relationship between human societies and their geological environment. As we continue to explore the implications of the neotectonic age, it becomes increasingly clear that our planet is a dynamic system, constantly evolving and presenting both challenges and opportunities for future generations.

“新构造时代”这一概念指的是地球的地壳在地质时间上受到显著影响的时期，特别是自晚新生代以来。理解“新构造时代”对地质学家和地球科学家至关重要，因为它提供了关于我们星球表面动态特性的洞察，并有助于预测地质灾害，如地震和火山喷发。“新构造”一词源于希腊语中的“neo”，意思是“新的”，而“构造”则与地球壳的结构和运动有关。因此，“新构造时代”涵盖了近期的地质历史，在这一时期，活跃的构造运动塑造了地貌并影响了沉积模式。在“新构造时代”期间，世界各地的不同地区由于构造板块的运动经历了显著的地质变化。例如，喜马拉雅山脉仍在上升，因为印度板块与欧亚板块相撞，这一过程自晚中生代以来一直在进行，但在“新构造时代”中加速。这种碰撞不仅形成了雄伟的山脉，还引发了可以导致毁灭性地震的地震活动。因此，研究“新构造时代”使科学家能够评估易发生自然灾害的地区的风险。此外，“新构造时代”的特点是各种地质特征的形成，包括断层、褶皱和裂谷。这些结构是由于构造力量造成的应力和应变在地壳中积累的结果。例如，加利福尼亚州的圣安德烈亚斯断层就是一个著名的转动断层，充分体现了该地区正在发生的活跃构造过程。通过分析在“新构造时代”形成的断层特征，研究人员可以更好地理解地震的机制，并制定更有效的减灾策略。除了在理解地质灾害方面的重要性外，“新构造时代”在资源管理中也发挥着重要作用。仍然处于构造活动状态的地区通常拥有丰富的自然资源，如矿产、石油和天然气。构造板块的运动可能导致这些资源的集中，使其具有经济价值。因此，了解“新构造时代”可以帮助探索和可持续管理这些资源，确保它们得到负责任地利用，而不会对环境造成伤害。此外，“新构造时代”的研究不仅限于地球科学；它还与考古学和人类学等领域交叉。许多古代文明在如今被认为是构造活跃区的地区发展。理解这些地区的地质历史可以为人类定居模式、农业实践甚至建筑风格提供背景。例如，在易发生地震的地区的古代城市遗址提供了关于韧性和适应自然灾害的宝贵教训，这在今天仍然具有相关性。总之，“新构造时代”是地质历史上一个重要的时期，反映了塑造我们星球的持续过程。其研究对于理解自然灾害、管理资源以及欣赏人类社会与地质环境之间的关系至关重要。随着我们继续探索“新构造时代”的影响，越来越清楚的是，我们的星球是一个动态系统，不断演变，为未来几代人带来了挑战和机遇。