lithostatic
简明释义
adj. 地压的,静岩的
英英释义
Relating to the pressure exerted by the weight of overlying rocks in geological contexts. | 与地质环境中上覆岩石的重量所施加的压力有关。 |
单词用法
岩石静态条件 | |
在岩石静态应力下 | |
计算岩石静压力 | |
测量岩石静载荷 |
同义词
反义词
例句
1.This paper mainly Outlines the new progress made in plate motion, lithostatic stress field, fault mechanics, active structure and long-term earthquake prediction.
文章主要对板块运动、岩石圈应力场、断层力学、活动构造、长期地震预测方面的新进展做了概略介绍。
2.This paper mainly Outlines the new progress made in plate motion, lithostatic stress field, fault mechanics, active structure and long-term earthquake prediction.
文章主要对板块运动、岩石圈应力场、断层力学、活动构造、长期地震预测方面的新进展做了概略介绍。
3.Geologists often measure lithostatic 岩石静压力 to understand the geological history of an area.
地质学家通常测量岩石静压力以了解某个地区的地质历史。
4.During tectonic activity, changes in lithostatic 岩石静压力 can lead to faulting.
在构造活动期间,岩石静压力的变化可能导致断层形成。
5.In sedimentary basins, the lithostatic 岩石静压力 increases with depth due to the accumulation of sediments.
在沉积盆地中,随着深度的增加,岩石静压力因沉积物的积累而增加。
6.The pressure exerted by the overlying rock layers is known as lithostatic 岩石静压力 pressure.
上覆岩层施加的压力被称为岩石静压力。
7.The concept of lithostatic 岩石静压力 is crucial for understanding subsurface fluid migration.
理解地下流体迁移时,岩石静压力的概念至关重要。
作文
The term lithostatic refers to the pressure exerted by the weight of overlying rocks in a geological context. This concept is crucial for understanding various geological processes, especially those that involve the formation and transformation of rocks beneath the Earth's surface. When we consider the layers of sedimentary rocks, the lithostatic pressure increases with depth due to the accumulation of material above. This pressure plays a significant role in the compaction and cementation of sediments, transforming them into solid rock over time.In many geological settings, the lithostatic pressure can influence the physical and chemical properties of rocks. For instance, as sediment accumulates and exerts more weight, the lithostatic pressure can lead to changes in mineral composition and grain size. This process is essential in the formation of various types of metamorphic rocks, where increased lithostatic pressure and temperature result in the recrystallization of minerals. Moreover, understanding lithostatic pressure is vital for geologists when studying tectonic movements. The Earth's crust is constantly shifting, and these movements can alter the distribution of lithostatic pressure in specific areas. For example, during mountain-building events, the weight of the newly formed mountains adds significant lithostatic pressure to the underlying crust. This can lead to phenomena such as faulting and folding, which are critical to understanding the dynamics of the Earth's surface.In addition to its geological implications, lithostatic pressure also has practical applications in fields such as petroleum engineering and mining. Engineers must consider lithostatic pressure when drilling for oil or gas, as the pressure can affect the flow of fluids within rock formations. Similarly, in mining operations, understanding the lithostatic pressure can help in designing safe and effective extraction methods.Overall, the concept of lithostatic pressure is fundamental in geology, influencing everything from rock formation to tectonic activity and resource extraction. By grasping the significance of lithostatic pressure, we can better appreciate the complex interactions that shape our planet's geology and contribute to the ongoing study of Earth sciences. As we continue to explore and learn about the Earth's processes, the role of lithostatic pressure will undoubtedly remain a key area of focus for geologists and researchers alike.In conclusion, the understanding of lithostatic pressure is not only essential for academic purposes but also for practical applications that impact industries reliant on geological resources. By appreciating the nuances of lithostatic pressure, we equip ourselves with the knowledge necessary to navigate the challenges and opportunities presented by the Earth's dynamic systems.
术语lithostatic指的是在地质背景下,由上覆岩石的重量施加的压力。这个概念对于理解各种地质过程至关重要,尤其是那些涉及地球表面下岩石的形成和转变的过程。当我们考虑沉积岩层时,随着深度的增加,lithostatic压力因上方物质的积累而增加。这种压力在沉积物的压实和胶结过程中发挥着重要作用,随着时间的推移,将其转变为固体岩石。在许多地质环境中,lithostatic压力可以影响岩石的物理和化学性质。例如,随着沉积物的积累并施加更多的重量,lithostatic压力可以导致矿物成分和颗粒大小的变化。这个过程对于各种类型的变质岩的形成至关重要,在这种情况下,增加的lithostatic压力和温度导致矿物的再结晶。此外,理解lithostatic压力对于地质学家研究构造运动至关重要。地球的地壳正在不断移动,这些运动可以改变特定区域内lithostatic压力的分布。例如,在山脉形成事件中,新形成山脉的重量会给底层地壳施加显著的lithostatic压力。这可能导致断层和褶皱等现象,这对于理解地球表面的动态至关重要。除了其地质意义外,lithostatic压力在石油工程和采矿等领域也具有实际应用。工程师在钻探石油或天然气时必须考虑lithostatic压力,因为这种压力可能影响岩石层内流体的流动。同样,在采矿操作中,理解lithostatic压力可以帮助设计安全有效的开采方法。总的来说,lithostatic压力的概念在地质学中是基础性的,影响从岩石形成到构造活动和资源开采的一切。通过掌握lithostatic压力的重要性,我们可以更好地欣赏塑造我们星球地质的复杂相互作用,并为持续研究地球科学做出贡献。随着我们继续探索和学习地球的过程,lithostatic压力的作用无疑将继续成为地质学家和研究人员关注的关键领域。最后,理解lithostatic压力不仅对学术目的至关重要,而且对依赖地质资源的行业产生影响的实际应用也同样重要。通过欣赏lithostatic压力的细微差别,我们为应对地球动态系统所带来的挑战和机遇提供了必要的知识。