orogenesis

简明释义

英[ˌɔːrəʊˈdʒenɪsɪs]美[ˌɔːroʊˈdʒenəsɪs]

n. 造山（运动）；山岳之形成

英英释义

单词用法

同义词

反义词

例句

1.The ore structure and generation of cobalt-gold ore minerals suggest that their formation mainly related to submarine sedimentary exhalation, reformed and mobilized in late collision orogenesis.

钴（金）矿石组构及矿石矿物的世代显示其主要与海底喷气沉积成矿作用有关，在后期的碰撞造山过程中，受到了改造和活化。

2.The ore structure and generation of cobalt-gold ore minerals suggest that their formation mainly related to submarine sedimentary exhalation, reformed and mobilized in late collision orogenesis.

钴（金）矿石组构及矿石矿物的世代显示其主要与海底喷气沉积成矿作用有关，在后期的碰撞造山过程中，受到了改造和活化。

3.Natural disasters and eco-environment in the Yangtze Valley have been restricted and impressed by crustal movement and Qinling-Dabie orogenesis since the Mesozoic and Cenozoic.

长江流域的地质-生态环境与自然灾害受到中新生代以来地壳运动和秦岭-大别等造山作用的严格制约与影响。

4.The origins of barrovian type and buchan type of metamorphism are commonly associated with orogenesis at continental collisional margins or within plates.

巴罗型中压变质带与巴肯型低压高温变质带的成因与大陆板块边缘的碰撞造山及陆内造山作用之间有着紧密的联系。

5.The collisional orogenesis in the area occurred in the Carboniferous and Permian, and shows the character of the early compression and late extension.

该区的碰撞造山作用主要发生在石炭纪和二叠纪，并经历了先挤压后伸展的演化过程。

6.The intrusion of magma affected the orogenesis and deformation and it is an important geological process and factor leading nonlinear deformation.

岩浆的侵入对造山变形有重要影响，同时也是导致区域非线性变形的重要地质过程和因素。

7.The alkali-syenites are of mantle-crust mixing type. The genesis of the rocks is associated with the orogenesis within the plate;

本区碱性正长岩类属幔壳混源成因类型，其成因与板内造山作用有关；

8.They occurred under the tectonic setting ranging from post collision uplift to late orogenesis.

产生于板块碰撞后隆起到造山晚期的构造背景。

9.The process of orogenesis is crucial for the formation of mountain ranges, such as the Himalayas.

地壳隆起的过程对于山脉的形成至关重要，例如喜马拉雅山。

10.Scientists study orogenesis to understand how tectonic plates interact and create new landforms.

科学家研究地壳隆起以了解构造板块如何相互作用并创造新的地貌。

11.The theory of orogenesis helps explain the geological history of regions like the Andes.

地壳隆起理论有助于解释安第斯山脉等地区的地质历史。

12.During orogenesis, immense pressure leads to the folding and faulting of Earth's crust.

在地壳隆起过程中，巨大的压力导致地球表层的褶皱和断裂。

13.The study of orogenesis provides insights into the processes that shape our planet's surface.

对地壳隆起的研究提供了对塑造我们星球表面过程的深入了解。

作文

Orogenesis is a fascinating geological process that refers to the formation of mountain ranges through tectonic forces and processes. This term, derived from the Greek words 'oros' meaning mountain and 'genesis' meaning creation, encapsulates a significant aspect of Earth's dynamic nature. Understanding orogenesis (造山作用) is crucial for geologists and earth scientists as it provides insights into the history of our planet's surface and the forces that shape it. The process of orogenesis begins with the movement of tectonic plates, which are large slabs of the Earth's lithosphere that float on the semi-fluid asthenosphere beneath. These plates can collide, pull apart, or slide past one another, leading to various geological phenomena. When two continental plates converge, they can create immense pressure that forces the land upwards, resulting in the formation of mountains. The Himalayas, for example, were formed as a result of the collision between the Indian Plate and the Eurasian Plate, a classic case of orogenesis (造山作用) in action. In addition to plate tectonics, erosion plays a significant role in shaping mountainous landscapes after their initial formation. As mountains rise, they are subjected to weathering and erosion from wind, water, and ice, which gradually sculpt their features over time. This interplay between orogenesis (造山作用) and erosion creates diverse ecosystems and habitats, influencing biodiversity and human settlements in mountainous regions. Furthermore, orogenesis (造山作用) is not a one-time event but a continuous process that can occur over millions of years. For instance, the Appalachian Mountains in North America have undergone several phases of orogenesis (造山作用) throughout their history, resulting in a complex geological structure that tells the story of ancient tectonic movements. Studying these mountain ranges allows scientists to piece together the geological history of our planet and understand how past events shape present-day landscapes. The significance of orogenesis (造山作用) extends beyond geology; it also has profound implications for climate, ecology, and human activity. Mountain ranges can act as barriers to weather patterns, influencing rainfall distribution and creating unique microclimates. This, in turn, affects the types of vegetation and wildlife that can thrive in these areas. Additionally, mountains are often rich in natural resources, such as minerals and forests, making them vital for human economies. However, the delicate balance of these ecosystems can be disrupted by activities such as mining, deforestation, and climate change, highlighting the need for sustainable practices in mountainous regions. In conclusion, orogenesis (造山作用) is a fundamental geological process that shapes our planet's surface and influences various aspects of life on Earth. By studying this phenomenon, we gain valuable insights into the Earth's history, the dynamics of its systems, and the interconnectedness of natural processes. As we continue to explore and understand the complexities of orogenesis (造山作用), we must also recognize our responsibility to protect these majestic landscapes for future generations.