breccia filling deposit

简明释义

角砾充填矿床;

英英释义

A breccia filling deposit is a geological formation consisting of angular fragments of rock that have been cemented together, typically found in sedimentary or volcanic environments.

角砾岩填充沉积物是一种地质构造,由角状岩石碎片组成,这些碎片通常在沉积或火山环境中被胶结在一起。

例句

1.Samples of the breccia filling deposit were taken for radiometric dating to determine its age.

角砾岩填充沉积物样本进行了放射性测年,以确定其年龄。

2.The formation of the breccia filling deposit was linked to the collapse of an ancient cave system.

角砾岩填充沉积物的形成与古老洞穴系统的崩塌有关。

3.The breccia filling deposit serves as a crucial indicator of tectonic movements in the region.

角砾岩填充沉积物是该地区构造运动的重要指示物。

4.During the excavation, workers encountered a large breccia filling deposit that required special handling.

在挖掘过程中,工人们遇到了一个大型的角砾岩填充沉积物,需要特别处理。

5.The geologist discovered a significant breccia filling deposit in the canyon, indicating past volcanic activity.

地质学家在峡谷中发现了一个重要的角砾岩填充沉积物,这表明过去有火山活动。

作文

The study of geological formations is a fascinating field that reveals much about the Earth's history. Among the various types of rock deposits, one particularly intriguing category is known as breccia filling deposit. A breccia filling deposit refers to a type of sedimentary rock that consists of angular fragments of pre-existing rocks or minerals. These fragments are typically cemented together by a finer-grained matrix, which can include clay, silt, or other materials. The formation of breccia filling deposits often occurs in environments where there has been significant geological activity, such as fault zones, volcanic eruptions, or landslides.Understanding the formation and significance of breccia filling deposits provides valuable insights into the processes that shape our planet. For instance, when tectonic plates shift, they can create fractures in the Earth's crust. Over time, these fractures may become filled with rock debris, resulting in the formation of breccia filling deposits. This process not only contributes to the diversity of rock types but also plays a crucial role in the geological history of an area.In addition to their formation, breccia filling deposits can serve as important indicators of past environmental conditions. Geologists often analyze these deposits to understand the dynamics of ancient landscapes. By studying the size, shape, and composition of the fragments within a breccia filling deposit, scientists can infer the intensity of geological events, such as earthquakes or volcanic eruptions, that may have occurred in the region.Moreover, breccia filling deposits can be found in various geological settings around the world, each offering unique insights into local geological history. For example, in mountainous regions, breccia filling deposits may form as a result of rockfall or landslide events, while in volcanic areas, they can occur due to explosive eruptions that fragment the surrounding rock. The study of these deposits not only enriches our understanding of geological processes but also aids in resource exploration, as certain types of breccia filling deposits can be associated with valuable minerals or fossil fuels.In conclusion, the term breccia filling deposit encapsulates a significant aspect of geological study, highlighting the dynamic processes that contribute to the formation of our planet's landscape. By examining these deposits, geologists can uncover the history of geological events and gain a deeper appreciation for the Earth's complexity. As we continue to explore and understand our planet, the study of breccia filling deposits will undoubtedly remain an essential component of geological research, shedding light on both the past and future of Earth’s geological evolution.

地质构造的研究是一个迷人的领域,它揭示了地球历史的许多方面。在各种岩石沉积类型中,有一种特别引人入胜的类别被称为角砾岩填充沉积角砾岩填充沉积是指由现有岩石或矿物的角状碎片组成的一种沉积岩。这些碎片通常被较细颗粒的基质粘结在一起,基质可以包括粘土、粉砂或其他材料。角砾岩填充沉积的形成通常发生在地质活动显著的环境中,如断层带、火山喷发或山崩。理解角砾岩填充沉积的形成及其重要性为我们提供了对塑造我们星球过程的宝贵见解。例如,当构造板块移动时,它们可以在地壳中产生裂缝。随着时间的推移,这些裂缝可能会被岩石残骸填充,从而形成角砾岩填充沉积。这一过程不仅促进了岩石类型的多样性,而且在一个地区的地质历史中也起着至关重要的作用。除了它们的形成,角砾岩填充沉积还可以作为过去环境条件的重要指标。地质学家经常分析这些沉积物,以了解古代景观的动态。通过研究角砾岩填充沉积内碎片的大小、形状和成分,科学家可以推测该地区可能发生的地震或火山喷发等地质事件的强度。此外,角砾岩填充沉积可以在世界各地的各种地质环境中找到,每种环境都提供了对当地地质历史的独特见解。例如,在山区,角砾岩填充沉积可能是由于落石或山崩事件而形成,而在火山地区,它们可能是由于爆炸性喷发破碎周围岩石而发生的。这些沉积物的研究不仅丰富了我们对地质过程的理解,还帮助资源勘探,因为某些类型的角砾岩填充沉积可能与有价值的矿物或化石燃料相关。总之,术语角砾岩填充沉积概括了地质研究的一个重要方面,突出了促成我们星球景观形成的动态过程。通过检查这些沉积物,地质学家可以揭示地质事件的历史,并更深入地欣赏地球的复杂性。随着我们继续探索和理解我们的星球,角砾岩填充沉积的研究无疑将继续成为地质研究的一个基本组成部分,照亮地球地质演变的过去和未来。

相关单词

filling

filling详解:怎么读、什么意思、用法