epeirogenic

简明释义

英[ˌɛpɪroʊˈdʒɛnɪk]美[ˌɛpɪroʊˈdʒɛnɪk]

造陆

英英释义

单词用法

同义词

反义词

例句

1.At present the reclamation epeirogenic's method has many, blows fills in the epeirogenic to save the cost, the reduction time aspect is without doubt in the numerous methods most effective.

目前填海造陆的方法有很多，吹填造陆在节约成本、缩短工期方面无疑是众多方法中最有效的一个。

2.At present the reclamation epeirogenic's method has many, blows fills in the epeirogenic to save the cost, the reduction time aspect is without doubt in the numerous methods most effective.

目前填海造陆的方法有很多，吹填造陆在节约成本、缩短工期方面无疑是众多方法中最有效的一个。

3.Angular unconformity belongs to an intraplate folded - orogenic deformation. Parallel unconformity is the record of intraplate epeirogenic deformation.

角度不整合是板内褶皱造山变形，平行不整合是板内造陆变形的重要记录。

4.Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour.

不同时期生成的盆地底板，将显示地壳构造的等级次序和造陆性质。

5.The epeirogenic 大陆隆起的 movements have significantly altered the landscape over millions of years.

这种epeirogenic 大陆隆起的运动在数百万年的时间里显著改变了地形。

6.Scientists study epeirogenic 大陆隆起的 processes to understand the geological history of the region.

科学家研究epeirogenic 大陆隆起的过程，以了解该地区的地质历史。

7.The epeirogenic 大陆隆起的 uplift in North America has created vast plateaus and mountain ranges.

北美的epeirogenic 大陆隆起的抬升形成了广阔的高原和山脉。

8.Understanding epeirogenic 大陆隆起的 phenomena is crucial for predicting future geological changes.

理解epeirogenic 大陆隆起的现象对预测未来的地质变化至关重要。

9.The epeirogenic 大陆隆起的 activity can lead to significant changes in river courses and ecosystems.

这种epeirogenic 大陆隆起的活动可能导致河流流向和生态系统的重大变化。

作文

The term epeirogenic refers to the geological processes that lead to the uplift or subsidence of large continental areas, without significant folding or faulting. Understanding epeirogenic movements is crucial for geologists and earth scientists as they study the long-term changes in the Earth's crust. These movements are typically slow and occur over millions of years, affecting vast regions rather than localized areas. For instance, the gradual uplift of the Colorado Plateau is a classic example of epeirogenic activity, where large sections of the Earth's crust rise uniformly without the dramatic effects of tectonic plate boundaries. In contrast to more dynamic geological processes, such as orogeny, which involves mountain building through intense folding and faulting, epeirogenic processes are often less visible yet equally significant. They can result from various factors, including the cooling and contraction of the Earth’s interior, sediment loading, and glacial rebound. For example, after the last Ice Age, many regions experienced epeirogenic uplift as glaciers melted and the weight on the land decreased. The implications of epeirogenic movements extend beyond geology; they also influence ecosystems, climate patterns, and human activities. As land rises or sinks, it can alter river courses, affect drainage patterns, and even impact weather conditions. This has profound consequences for agriculture, urban planning, and natural resource management. In areas undergoing significant epeirogenic uplift, new habitats may form, while other regions may become more prone to flooding or erosion. Moreover, the study of epeirogenic movements aids in understanding past geological events and predicting future changes. By analyzing sediment layers and fossil records, scientists can infer the historical context of these movements. This information is vital for assessing risks associated with natural disasters, such as earthquakes and landslides, which can be influenced by underlying epeirogenic processes. In conclusion, the concept of epeirogenic movements encompasses a range of geological phenomena that shape our planet's surface over extensive periods. While they may not capture the immediate attention like volcanic eruptions or earthquakes, their long-term effects are fundamental in understanding the Earth's evolution. As we continue to explore and study these processes, we gain deeper insights into the intricate systems that govern our planet's geology and its impact on life as we know it.

造陆的一词指的是导致大面积大陆地区隆起或沉降的地质过程，而没有显著的褶皱或断层。理解造陆的运动对地质学家和地球科学家来说至关重要，因为他们研究地壳的长期变化。这些运动通常是缓慢的，发生在数百万年中，影响广泛区域而非局部区域。例如，科罗拉多高原的逐渐隆起就是造陆的活动的经典例子，其中大片地壳均匀上升，而没有板块边界的剧烈影响。 与更动态的地质过程相比，如造山运动，它涉及通过强烈的褶皱和断层形成山脉，造陆的过程通常不那么明显，但同样重要。它们可以由多种因素引起，包括地球内部的冷却和收缩、沉积物负荷以及冰川反弹。例如，在上一个冰河时代之后，许多地区经历了造陆的隆起，因为冰川融化，土地上的重量减少。 造陆的运动的影响超越了地质学；它们还影响生态系统、气候模式和人类活动。随着土地的隆起或下沉，它可能改变河流的流向，影响排水模式，甚至影响天气条件。这对农业、城市规划和自然资源管理有深远的影响。在经历显著造陆的隆起的地区，新的栖息地可能会形成，而其他地区可能更容易遭受洪水或侵蚀。 此外，研究造陆的运动有助于理解过去的地质事件并预测未来的变化。通过分析沉积层和化石记录，科学家可以推断这些运动的历史背景。这些信息对于评估与自然灾害相关的风险至关重要，例如地震和滑坡，这些都可能受到潜在的造陆的过程的影响。 总之，造陆的运动的概念包含了一系列塑造我们星球表面的地质现象，历时漫长。虽然它们可能不像火山喷发或地震那样立即引起注意，但它们的长期影响对理解地球的演变至关重要。随着我们继续探索和研究这些过程，我们将更深入地了解支配我们星球地质及其对生命影响的复杂系统。