anorogenic time

简明释义

1. 非造山期; 2. 非造山运动时期;

英英释义

Anorogenic time refers to a geological period characterized by a lack of significant tectonic activity, where there is minimal mountain building or volcanic activity.

无造山期是指一个地质时期,其特征是缺乏显著的构造活动,几乎没有山脉形成或火山活动。

例句

1.The formation of sedimentary rocks is often linked to processes occurring in an anorogenic time 无造山时间.

沉积岩的形成通常与发生在无造山时间 无造山时间的过程有关。

2.Studying fossils from the anorogenic time 无造山时间 can provide insights into ancient ecosystems.

研究来自无造山时间 无造山时间的化石可以提供对古代生态系统的见解。

3.The stability of the continental crust is often attributed to its long history of anorogenic time 无造山时间.

大陆地壳的稳定性通常归因于其悠久的无造山时间 无造山时间历史。

4.Many mineral deposits are formed as a result of geological processes during anorogenic time 无造山时间.

许多矿产资源是由于在无造山时间 无造山时间期间的地质过程而形成的。

5.During the geological survey, we discovered that this region experienced significant changes during the anorogenic time 无造山时间.

在地质调查中,我们发现该地区在无造山时间 无造山时间经历了重大变化。

作文

The concept of anorogenic time refers to periods in geological history when there is little to no tectonic activity, leading to a relative stability in the Earth's crust. During these times, the landscape undergoes significant erosion and sedimentation processes, shaping the features we see today. Understanding anorogenic time is crucial for geologists as it helps them reconstruct past environments and predict future geological changes.In many ways, anorogenic time can be seen as a time of peace for the Earth’s crust. Unlike tectonically active periods characterized by earthquakes, volcanic eruptions, and mountain-building, these calm intervals allow for the gradual wearing down of mountains and the filling of basins with sediments. For instance, the Appalachian Mountains, which were once towering peaks, have been significantly eroded during various anorogenic times, resulting in the rolling hills we see today.Moreover, anorogenic time plays a vital role in the formation of sedimentary rocks. As rivers carry sediments from higher elevations to lower areas, these materials accumulate over time, eventually compacting and cementing into rock. This process not only contributes to the geological record but also provides valuable resources such as coal, oil, and natural gas. The understanding of these processes is essential for resource exploration and environmental management.In addition to its geological significance, anorogenic time can also be metaphorically applied to our lives. Just as the Earth experiences periods of stability, humans also go through phases where life seems to be calm and predictable. These times can be viewed as opportunities for growth and reflection. For example, during an anorogenic time in one’s career, an individual might focus on personal development, skill enhancement, or nurturing relationships without the distractions of sudden changes or upheavals.On a broader scale, societies experience anorogenic times in the context of political stability and economic growth. Periods of peace often lead to advancements in culture, technology, and social structures. For instance, the Renaissance was marked by a relatively stable European continent, allowing for unprecedented developments in art, science, and philosophy. Similarly, in modern times, nations that enjoy long periods of peace tend to flourish economically and socially.In conclusion, the study of anorogenic time provides valuable insights into geological processes and human experiences. By examining these periods of stability, we can better understand the Earth's history and appreciate the moments of calm in our own lives. Whether on a geological scale or within our personal journeys, recognizing the importance of anorogenic time encourages us to embrace stability as a foundation for growth and transformation.

无造山时期”的概念指的是地质历史中几乎没有构造活动的时期,这导致地壳相对稳定。在这些时间里,景观经历了显著的侵蚀和沉积过程,塑造了我们今天所看到的特征。理解无造山时期对地质学家至关重要,因为它帮助他们重建过去的环境,并预测未来的地质变化。在许多方面,无造山时期可以被视为地球地壳的和平时期。与以地震、火山喷发和造山运动为特征的构造活跃时期不同,这些平静的间隔允许山脉逐渐被侵蚀,盆地被沉积物填满。例如,阿巴拉契亚山脉曾经是高耸的山峰,但在多个无造山时期中经历了显著的侵蚀,导致我们今天看到的起伏丘陵。此外,无造山时期在沉积岩的形成中也发挥着重要作用。随着河流将沉积物从高处带到低洼地区,这些材料随着时间的推移而积累,最终压实并固结成岩石。这一过程不仅有助于地质记录的形成,还提供了煤、石油和天然气等宝贵资源。理解这些过程对资源勘探和环境管理至关重要。除了其地质意义外,无造山时期还可以隐喻性地应用于我们的生活。正如地球经历稳定时期一样,人类也会经历生活中看似平静和可预测的阶段。这些时期可以被视为成长和反思的机会。例如,在个人职业生涯中的无造山时期,个人可能会专注于个人发展、技能提升或培养关系,而不受突发变化或动荡的干扰。在更广泛的范围内,社会在政治稳定和经济增长的背景下也经历无造山时期。和平时期往往导致文化、科技和社会结构的进步。例如,文艺复兴时期以相对稳定的欧洲大陆为标志,允许艺术、科学和哲学方面的前所未有的发展。类似地,在现代,享有长时间和平的国家往往在经济和社会上繁荣。总之,对无造山时期的研究提供了对地质过程和人类经历的宝贵见解。通过考察这些稳定的时期,我们可以更好地理解地球的历史,并欣赏我们自己生活中的平静时刻。无论是在地质规模还是在个人旅程中,认识到无造山时期的重要性鼓励我们拥抱稳定,作为成长和转变的基础。