orogeny

简明释义

英[ɒˈrɒdʒəni]美[ɔːˈrɑːdʒəni]

n. [地质] 造山运动，造山作用；山岳的形成

英英释义

单词用法

同义词

反义词

例句

1.The collision orogeny is a uniformitive process after the collision event.

碰撞造山作用是一个在碰撞事件之后的均变过程。

2.The period was one of general emergence and orogeny.

这个时期是全面的上升和造山运动。

3.Since the Permian, the Tarim Basin had undergone basinal extension, subduction and intro-continental orogeny.

塔里木盆地自二叠纪以来，历经盆地扩张和盆地俯冲以及陆内造山作用的过程。

4.In the late Yanshan orogeny, this area was characterized by brittle fracture.

燕山晚期本区以脆性构造为主，断裂构造发育。

5.The effective traps for petroleum accumulation were developed mainly in late Yanshan orogeny.

燕山晚期运动为本区的油气聚集提供了有效的圈闭。

6.Foreland basins are the key areas for the study of orogeny.

前陆盆地是研究造山运动的关键地区之一。

7.Velocity values beneath Sulu region and the Shandong peninsula are in the identical contour line with that beneath the Dabie orogeny belt.

苏鲁、山东半岛下面的速度分布与大别造山带下面的速度分布处于同一个速度等值区域上。

8.The end of the sedimentation of the foreland basin indicates completion of the collisional orogeny .

前陆盆地的终结标志着碰撞造山作用的结束。

9.As a typical orogeny of continental collision, Qingling has no condition for large scale UHPM formation, although scattered UHPM may not be excluded.

秦岭作为典型造山带，虽然不排除零星超高压变质的可能，但不具备大规模超高压变质的条件。

10.The Himalayas were formed as a result of intense orogeny.

喜马拉雅山脉是由于剧烈的造山运动而形成的。

11.Geologists study orogeny to understand mountain-building processes.

地质学家研究造山运动以理解山脉形成的过程。

12.The concept of orogeny is crucial in plate tectonics.

在板块构造中，造山运动的概念至关重要。

13.Ongoing orogeny can lead to earthquakes in mountainous regions.

持续的造山运动可能导致山区发生地震。

14.The study of orogeny helps predict geological hazards.

对造山运动的研究有助于预测地质灾害。

作文

The Earth is a dynamic planet, constantly changing and evolving due to various geological processes. One of the most significant processes that shape our planet's surface is orogeny, which refers to the process of mountain formation, particularly through tectonic plate movements. This phenomenon not only creates majestic mountain ranges but also plays a crucial role in influencing climate, biodiversity, and human activities. Understanding orogeny is essential for geologists and environmentalists alike, as it provides insights into the Earth's history and its ongoing transformations. Orogens, or mountain ranges formed through orogeny, can be classified into different types based on their formation mechanisms. The most common type occurs at convergent plate boundaries, where two tectonic plates collide. This collision often results in the folding and faulting of the Earth's crust, leading to the uplift of land and the creation of mountains. For instance, the Himalayas, which are home to Mount Everest, were formed as a result of the collision between the Indian Plate and the Eurasian Plate. This dramatic event showcases the power of orogeny in shaping the landscape. In addition to the physical changes that orogeny brings about, it also has profound effects on the environment. Mountain ranges influence weather patterns by acting as barriers to prevailing winds, which can lead to varied climates on either side of the range. For example, the Andes Mountains in South America create a rain shadow effect, resulting in lush vegetation on the western slopes while the eastern side remains arid. Such climatic variations foster diverse ecosystems, making regions around orogenic areas rich in biodiversity. Moreover, orogeny has significant implications for human societies. Historically, many civilizations have thrived in mountainous regions due to the natural resources they provide, such as minerals, forests, and fertile soil. However, these areas can also pose challenges, including landslides, earthquakes, and volcanic activity, which are often associated with ongoing orogeny. Therefore, understanding the processes behind mountain formation is vital for disaster preparedness and sustainable development. Furthermore, the study of orogeny contributes to our knowledge of plate tectonics, a fundamental theory in geology that explains the movement of the Earth's lithosphere. By examining the characteristics of different mountain ranges and the forces that created them, scientists can reconstruct past geological events and predict future changes. This research is not only important for academic purposes but also for practical applications, such as resource management and environmental conservation. In conclusion, orogeny is a fascinating and complex process that significantly impacts our planet's landscape, climate, and ecosystems. It exemplifies the intricate interplay between geological forces and the environment, highlighting the importance of understanding these processes in our quest to protect and preserve the Earth. As we continue to explore the mysteries of orogeny, we gain valuable insights into the Earth's past, present, and future, ultimately enriching our appreciation for the natural world around us.

地球是一个动态的星球，由于各种地质过程不断变化和演化。其中一个对我们星球表面形状影响最显著的过程是造山作用，指的是山脉形成的过程，特别是通过构造板块运动。这种现象不仅创造了壮丽的山脉，而且在影响气候、生物多样性和人类活动方面发挥着至关重要的作用。理解造山作用对地质学家和环境学家来说至关重要，因为它提供了对地球历史及其持续变革的见解。 造山带，即通过造山作用形成的山脉，可以根据其形成机制分为不同类型。最常见的一种发生在汇聚板块边界，当两个构造板块相撞时。这种碰撞通常导致地壳的褶皱和断裂，导致土地的抬升和山脉的形成。例如，喜马拉雅山脉，包括珠穆朗玛峰，是由于印度板块与欧亚板块的碰撞而形成的。这一戏剧性的事件展示了造山作用在塑造地貌方面的力量。 除了造山作用带来的物理变化外，它对环境也有深远的影响。山脉通过充当盛行风的障碍物来影响天气模式，这可能导致山脉两侧气候的差异。例如，南美洲的安第斯山脉造成了雨影效应，导致西侧植被茂盛，而东侧则保持干旱。这种气候变化促进了多样的生态系统，使得造山地区周围的区域生物多样性丰富。 此外，造山作用对人类社会具有重要意义。历史上，许多文明因山区提供的自然资源（如矿产、森林和肥沃的土壤）而繁荣。然而，这些地区也可能带来挑战，包括滑坡、地震和火山活动，这些往往与持续的造山作用有关。因此，理解山脉形成背后的过程对于灾害准备和可持续发展至关重要。 此外，造山作用的研究有助于我们了解板块构造，这是地质学中的一个基本理论，解释了地球岩石圈的运动。通过检查不同山脉的特征和创建它们的力量，科学家可以重建过去的地质事件并预测未来的变化。这项研究不仅对学术目的重要，而且对资源管理和环境保护等实际应用也至关重要。 总之，造山作用是一个迷人而复杂的过程，对我们星球的地貌、气候和生态系统产生了重大影响。它例证了地质力量与环境之间错综复杂的相互作用，突显了理解这些过程在保护和维护地球方面的重要性。随着我们继续探索造山作用的奥秘，我们获得了对地球过去、现在和未来的宝贵见解，最终丰富了我们对周围自然世界的欣赏。