aqueous rock

简明释义

水成岩;

英英释义

例句

1.The study focused on the mineral composition of aqueous rock 水成岩 found in sedimentary layers.

该研究集中于在沉积层中发现的水成岩 aqueous rock 的矿物组成。

2.The presence of aqueous rock 水成岩 can indicate past water activity in geological surveys.

在地质调查中，水成岩 aqueous rock 的存在可以表明过去的水活动。

3.During the field trip, we collected samples of aqueous rock 水成岩 from the riverbed.

在实地考察中，我们从河床收集了水成岩 aqueous rock 的样本。

4.The geologist explained that the formation of aqueous rock 水成岩 occurs primarily in underwater environments.

地质学家解释说，水成岩 aqueous rock 的形成主要发生在水下环境中。

5.Researchers found that aqueous rock 水成岩 plays a crucial role in the ecosystem by providing habitats for aquatic life.

研究人员发现，水成岩 aqueous rock 在生态系统中发挥着重要作用，为水生生物提供栖息地。

作文

The study of geology encompasses various aspects of the Earth's structure, including the formation and classification of different types of rocks. Among these classifications, one particularly intriguing category is referred to as aqueous rock, which denotes rocks that have formed in environments influenced by water. Understanding aqueous rock is essential for geologists, as it provides insights into the historical climate conditions and geological processes that have shaped our planet. Aqueous rocks primarily include sedimentary rocks, which are created from the accumulation of sediments transported by water. These sediments can consist of minerals, organic materials, and other debris that settle at the bottom of oceans, rivers, and lakes. Over time, the pressure from overlying materials compacts these sediments, leading to the formation of rocks such as sandstone, limestone, and shale. Each type of aqueous rock tells a unique story about the environment in which it was formed. For example, limestone, a common type of aqueous rock, often forms in shallow marine environments where organisms like corals and shellfish thrive. The accumulation of their shells and skeletal remains contributes to the limestone's composition. This rock not only serves as a valuable resource for construction and manufacturing but also acts as a crucial indicator of past marine conditions. By studying limestone deposits, scientists can infer changes in sea levels, water temperatures, and even the types of organisms that existed millions of years ago. In contrast, sandstone is another type of aqueous rock that generally forms from sand-sized particles that have been cemented together by minerals precipitated from water. Sandstone is prevalent in desert environments and riverbeds, showcasing the dynamic nature of water flow and sediment transport. The characteristics of sandstone can vary widely depending on its source material, cementing agents, and the conditions under which it formed. Geologists often analyze sandstone to understand ancient landscapes and the processes that shaped them. The significance of aqueous rock extends beyond mere classification; it plays a vital role in natural resource management and environmental studies. For instance, many aquifers, which are crucial sources of freshwater, are found within porous aqueous rock formations. Understanding the permeability and porosity of these rocks helps in managing water resources effectively. Moreover, the study of aqueous rock can aid in identifying potential sites for oil and gas extraction, as these resources are often trapped within sedimentary layers. In conclusion, aqueous rock is a fundamental concept in geology that encompasses various sedimentary rocks formed in water-influenced environments. By examining these rocks, scientists can unravel the history of our planet, understand past climates, and manage vital natural resources. As we continue to explore the complexities of Earth’s geology, the importance of aqueous rock will undoubtedly remain a key focus for researchers and environmentalists alike.

地质学的研究涵盖了地球结构的各个方面，包括不同类型岩石的形成和分类。在这些分类中，有一个特别引人入胜的类别被称为水成岩，指的是在受水影响的环境中形成的岩石。理解水成岩对地质学家至关重要，因为它提供了关于塑造我们星球的历史气候条件和地质过程的见解。水成岩主要包括沉积岩，这些岩石是由水运输的沉积物的积累而形成的。这些沉积物可以由矿物、有机材料和其他沉淀物组成，这些沉淀物在海洋、河流和湖泊的底部沉积。随着时间的推移，上覆材料的压力使这些沉积物压实，从而形成砂岩、石灰岩和页岩等岩石。每种类型的水成岩都讲述了一个关于其形成环境的独特故事。例如，石灰岩是一种常见的水成岩，通常在浅海环境中形成，在那里，珊瑚和贝类等生物繁盛。它们的壳体和骨骼残骸的积累构成了石灰岩的成分。这种岩石不仅是建筑和制造的重要资源，而且还作为过去海洋条件的重要指标。通过研究石灰岩沉积物，科学家可以推断出海平面、水温甚至数百万年前存在的生物类型的变化。相反，砂岩是另一种类型的水成岩，通常由沙粒大小的颗粒组成，这些颗粒通过从水中沉淀出来的矿物粘结在一起。砂岩在沙漠环境和河床中很常见，展示了水流动和沉积运输的动态特性。砂岩的特征可能因其源材料、粘结剂和形成条件的不同而有很大差异。地质学家经常分析砂岩，以了解古代景观及其塑造过程。水成岩的重要性超越了简单的分类；它在自然资源管理和环境研究中发挥着至关重要的作用。例如，许多含水层——这些是重要的淡水来源——存在于多孔的水成岩层中。了解这些岩石的渗透性和孔隙率有助于有效管理水资源。此外，对水成岩的研究可以帮助识别潜在的石油和天然气开采地点，因为这些资源通常被困在沉积层中。总之，水成岩是地质学中的一个基本概念，涵盖了在受水影响的环境中形成的各种沉积岩。通过检查这些岩石，科学家可以揭示我们星球的历史，了解过去的气候，并管理重要的自然资源。随着我们继续探索地球地质的复杂性，水成岩的重要性无疑将继续成为研究人员和环保主义者的重点关注。