analcime dolerite

简明释义

方沸石粒玄岩;

英英释义

例句

1.The unique mineral composition of analcime dolerite 方沸石辉绿岩 makes it an interesting subject for petrological studies.

由于其独特的矿物组成，analcime dolerite 方沸石辉绿岩成为岩石学研究的一个有趣课题。

2.The geological survey revealed that the region is rich in analcime dolerite 方沸石辉绿岩, which may indicate volcanic activity in the past.

地质调查显示该地区富含analcime dolerite 方沸石辉绿岩, 这可能表明过去有火山活动。

3.Samples of analcime dolerite 方沸石辉绿岩 were collected for further analysis in our lab.

我们在实验室收集了analcime dolerite 方沸石辉绿岩样本以进行进一步分析。

4.The presence of analcime dolerite 方沸石辉绿岩 can affect the local soil composition and fertility.

analcime dolerite 方沸石辉绿岩的存在可能会影响当地土壤的成分和肥力。

5.In some regions, analcime dolerite 方沸石辉绿岩 is used as a decorative stone in landscaping.

在某些地区，analcime dolerite 方沸石辉绿岩被用作园林美化中的装饰石材。

作文

The study of geology often reveals a fascinating world beneath our feet, where various minerals and rocks tell a story of the Earth's history. One such intriguing rock type is analcime dolerite, which is a variety of dolerite that contains the mineral analcime. Dolerite itself is an igneous rock, typically formed from the cooling of magma, and is known for its coarse-grained texture. The addition of analcime, a zeolite mineral, adds unique properties to this rock, making it a subject of interest for both geologists and mineralogists.To understand analcime dolerite, we first need to explore its components. Dolerite is primarily composed of plagioclase feldspar, pyroxene, and sometimes olivine. These minerals crystallize from magma as it cools slowly beneath the Earth's surface. However, when conditions are right, analcime can form within the dolerite matrix, usually in the presence of alkaline fluids. This process can occur during the later stages of cooling or through hydrothermal activity, where hot, mineral-rich water interacts with the rock.The presence of analcime in analcime dolerite significantly influences its properties. Analcime is characterized by its ability to absorb water and other ions, which can lead to changes in the rock’s physical and chemical characteristics. This hydrous mineral can also affect the rock's porosity and permeability, making it more interesting for studies related to groundwater movement and resource extraction.Geologically, analcime dolerite can be found in various locations around the world, often associated with volcanic activity or areas where ancient lava flows have cooled. Its formation is indicative of specific environmental conditions that were present at the time of its creation. Studying these rocks can provide insights into past geological events, including volcanic eruptions and tectonic movements.In terms of practical applications, analcime dolerite is not just a subject of academic interest; it also has implications in the fields of engineering and construction. The durability and strength of dolerite make it a favored material for building roads, railways, and other infrastructure. When analcime is present, it can enhance certain properties, such as resistance to weathering and erosion, further increasing its utility in construction projects.Moreover, the presence of analcime can impact the economic value of dolerite deposits. Mining companies may seek out analcime dolerite for its mineral content, which can be beneficial in various industrial processes. Understanding the distribution and characteristics of this rock type can lead to more efficient extraction methods and better resource management.In conclusion, analcime dolerite is a remarkable rock type that embodies the complex interplay of geological processes. Its unique composition and properties make it a valuable subject for research and practical applications alike. As we continue to explore the Earth's geology, rocks like analcime dolerite remind us of the dynamic nature of our planet and the stories that lie within its depths.

地质学的研究常常揭示出我们脚下迷人的世界，各种矿物和岩石讲述着地球历史的故事。其中一种引人入胜的岩石类型是分析石辉长岩，它是一种含有分析石矿物的辉长岩。辉长岩本身是一种火成岩，通常由岩浆冷却形成，以其粗颗粒的纹理而闻名。分析石的加入，这是一种沸石矿物，为这种岩石增添了独特的特性，使其成为地质学家和矿物学家的研究对象。要理解分析石辉长岩，我们首先需要探讨其组成。辉长岩主要由斜长石、辉石，有时还有橄榄石组成。这些矿物在岩浆缓慢冷却时结晶。然而，当条件合适时，分析石可以在辉长岩基质中形成，通常是在碱性流体的存在下。这一过程可能发生在冷却的后期阶段，或通过热液活动，即热的富含矿物的水与岩石相互作用。分析石在分析石辉长岩中的存在显著影响其特性。分析石的特点是能够吸收水分和其他离子，这可能导致岩石的物理和化学特性发生变化。这种含水矿物还可以影响岩石的孔隙度和渗透性，使其在与地下水运动和资源开采相关的研究中更加有趣。从地质学的角度来看，分析石辉长岩可以在世界各地的不同地点找到，通常与火山活动或古老熔岩流的冷却有关。它的形成表明在其创造时存在特定的环境条件。研究这些岩石可以提供对过去地质事件的见解，包括火山喷发和构造运动。在实际应用方面，分析石辉长岩不仅是学术兴趣的主题；它在工程和建筑领域也有重要意义。辉长岩的耐久性和强度使其成为建造道路、铁路和其他基础设施的理想材料。当分析石存在时，它可以增强某些特性，例如抵抗风化和侵蚀的能力，进一步增加其在建设项目中的效用。此外，分析石的存在可以影响辉长岩矿床的经济价值。采矿公司可能会寻找分析石辉长岩以获取其矿物成分，这在各种工业过程中可能是有益的。了解这种岩石类型的分布和特征可以导致更有效的开采方法和更好的资源管理。总之，分析石辉长岩是一种非凡的岩石类型，体现了地质过程的复杂相互作用。其独特的组成和特性使其成为研究和实际应用的宝贵主题。随着我们继续探索地球的地质，像分析石辉长岩这样的岩石提醒着我们星球的动态特性以及隐藏在其深处的故事。