lithify

简明释义

英[ˈlɪθɪfaɪ]美[ˈlɪθəˌfaɪ]

岩化

英英释义

单词用法

同义词

反义词

例句

1.This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

这块石头包含石髓的水泥之前，它经历了岩化作用，一个过程，那里的低温和低的压力，改变的内容，沉积物之前，他们终于岩化，或变成岩石。

2.This rock contained chalcedonic cement before it underwent diagenesis, a process where low temperatures and low pressures alter the content of sediments before they finally lithify, or turn into rock.

这块石头包含石髓的水泥之前，它经历了岩化作用，一个过程，那里的低温和低的压力，改变的内容，沉积物之前，他们终于岩化，或变成岩石。

3.To that end, it is working to build a press that can apply "compressive forces so great as to actually lithify mineral grains, turning loose sediment into stone, " according to its news release.

为此，根据他的新闻发布，它将会建立一个压力以适用“足够大的压力以至于将实际岩化的矿物颗粒变成石头”。

4.Sands lithify into sandstones.

砂经过石化而成砂岩。

5.The transformation of loose sand into sandstone occurs when it lithifies.

当松散的沙子成岩时，会转变为砂岩。

6.Over millions of years, sediments can lithify into solid rock.

经过数百万年，沉积物可以成岩为坚固的岩石。

7.Geologists study how different conditions affect the rate at which sediments lithify.

地质学家研究不同条件如何影响沉积物成岩的速度。

8.The process by which mud can lithify is essential in the formation of shale.

泥土如何成岩的过程对于页岩的形成至关重要。

9.As the layers of sediment build up, they eventually lithify under pressure.

随着沉积层的堆积，它们最终在压力下成岩。

作文

The process of sedimentary rock formation is fascinating and complex, involving numerous geological phenomena. One of the key processes in this transformation is known as lithify, which refers to the process by which sediments compact under pressure and gradually become solid rock. This process can take thousands to millions of years, depending on various factors such as the type of sediment, environmental conditions, and the presence of minerals that aid in cementation. Understanding how sediments lithify helps us appreciate the dynamic nature of our planet's surface and the history recorded in its layers.Sediments are typically formed from the weathering and erosion of pre-existing rocks. Over time, these particles accumulate in various environments, such as riverbeds, lakes, and ocean floors. As more sediments pile up, the weight of the overlying material exerts pressure on the layers below. This pressure causes the sediments to compact, reducing the space between the particles. During this compaction process, water that was originally trapped between the grains is expelled, and minerals dissolved in the water may precipitate and fill the gaps, effectively gluing the particles together. This cementation is a crucial aspect of how sediments lithify into solid rock.There are several types of sedimentary rocks formed through the lithify process, including sandstone, limestone, and shale. Sandstone, for example, is primarily composed of sand-sized particles that have undergone significant compaction and cementation. Limestone often forms from the accumulation of organic materials, like shells and coral, which also undergo lithify to create a dense rock. Similarly, shale is formed from fine particles of clay that have compacted and hardened over time. Each of these rocks tells a unique story about the environment in which they formed, providing valuable insights into Earth's history.The study of how sediments lithify is not only important for geologists but also has practical applications in fields such as construction, natural resource extraction, and environmental science. For instance, understanding the properties of sedimentary rocks can help engineers assess the stability of a site for building projects. Additionally, the knowledge gained from studying lithify processes can aid in locating fossil fuels and groundwater resources, which are crucial for modern society.In conclusion, the term lithify encapsulates a fundamental geological process that transforms loose sediments into solid rock. By exploring this concept, we gain a deeper appreciation for the intricate processes that shape our planet. The formation of sedimentary rocks through lithify not only provides a record of Earth’s history but also plays a significant role in various scientific and practical applications. As we continue to study and understand these processes, we uncover the stories written in the layers of rock beneath our feet, reminding us of the ever-changing nature of the Earth we inhabit.

沉积岩的形成过程既迷人又复杂，涉及许多地质现象。在这个转变过程中，一个关键的过程被称为lithify，它指的是沉积物在压力下压实并逐渐变成固体岩石的过程。根据沉积物的类型、环境条件以及促进胶结的矿物的存在，这一过程可能需要数千到数百万年。理解沉积物如何lithify有助于我们欣赏地球表面的动态特性以及其层次中记录的历史。沉积物通常是由已有岩石的风化和侵蚀形成的。随着时间的推移，这些颗粒在河床、湖泊和海洋底部等各种环境中积累。随着更多沉积物的堆积，上覆物质的重量对下面的层施加压力。这种压力导致沉积物压实，减少颗粒之间的空间。在这一压实过程中，原本被困在颗粒之间的水被挤出，溶解在水中的矿物质可能会沉淀并填充空隙，有效地将颗粒粘合在一起。胶结过程是沉积物如何lithify成固体岩石的关键方面。通过lithify过程形成的几种类型的沉积岩，包括砂岩、石灰岩和页岩。例如，砂岩主要由经过显著压实和胶结的沙粒组成。石灰岩通常由有机材料的积累形成，如贝壳和珊瑚，这些材料也经历lithify形成致密的岩石。同样，页岩是由细小的粘土颗粒在时间的推移下压实和硬化而成的。这些岩石中的每一种都讲述了它们形成时环境的独特故事，为我们提供了关于地球历史的宝贵见解。研究沉积物如何lithify不仅对地质学家重要，还有助于建筑、自然资源开采和环境科学等领域的实际应用。例如，了解沉积岩的性质可以帮助工程师评估建筑项目的场地稳定性。此外，从研究lithify过程获得的知识可以帮助定位化石燃料和地下水资源，这对现代社会至关重要。总之，术语lithify概括了一种基本的地质过程，将松散的沉积物转变为固体岩石。通过探索这一概念，我们更深入地理解塑造我们星球的复杂过程。通过lithify形成的沉积岩不仅提供了地球历史的记录，还在各种科学和实际应用中发挥着重要作用。随着我们继续研究和理解这些过程，我们揭示了脚下岩石层中写下的故事，提醒我们所居住的地球的不断变化。