anorthic

简明释义

英[ænˈɔːθɪk]美[æˈnɔrθɪk]

adj. （晶体）三斜的

英英释义

单词用法

同义词

反义词

例句

1.The albite component increases while anorthic component decreases in detrital plagioclase. The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组分逐渐增多，钙长石组分逐渐减少，最终形成纯钠端元的钠长石。

2.The albite component increases while anorthic component decreases in detrital plagioclase. The plagioclase turned into an end - member component of albite.

斜长石碎屑中钠长石组分逐渐增多，钙长石组分逐渐减少，最终形成纯钠端元的钠长石。

3.Some gemstones exhibit anorthic properties, making them valuable for collectors.

一些宝石表现出无方晶系特性，使它们对收藏家来说很有价值。

4.The researchers noted that the anorthic nature of the sample indicated a high degree of symmetry.

研究人员指出，样品的无方晶系特性表明其对称性很高。

5.The crystal structure of the mineral is classified as anorthic, which means it has a unique arrangement of atoms.

这种矿物的晶体结构被归类为无方晶系，这意味着它具有独特的原子排列。

6.In geology, understanding anorthic systems can help in identifying various rock types.

在地质学中，理解无方晶系系统有助于识别各种岩石类型。

7.The study focused on anorthic minerals found in the region's volcanic rocks.

这项研究集中在该地区火山岩中发现的无方晶系矿物上。

作文

The concept of anorthic crystals is fascinating and plays a significant role in the field of mineralogy. Anorthic, defined as having a crystal system that lacks symmetry, can be seen in various minerals that exhibit unique properties due to their structural characteristics. Understanding the implications of anorthic (无对称的) structures helps geologists and material scientists to decipher the formation processes of these minerals and their potential applications. In the world of geology, the classification of minerals is crucial. Minerals are categorized based on their crystal systems, which include cubic, tetragonal, hexagonal, orthorhombic, monoclinic, and anorthic (无对称的). Each system has distinct symmetry elements that define its shape and properties. The anorthic (无对称的) system is particularly intriguing because it does not possess the symmetrical features found in other crystal systems.One of the most notable examples of anorthic (无对称的) minerals is plagioclase feldspar, a common component in many igneous rocks. This mineral exhibits a range of compositions and can display varying degrees of anorthic (无对称的) characteristics. The study of such minerals reveals much about the geological history of an area, including the conditions under which the rocks formed.Furthermore, the anorthic (无对称的) nature of certain minerals can influence their physical properties, such as hardness, cleavage, and optical characteristics. For instance, the lack of symmetry in anorthic (无对称的) crystals can lead to unique light refraction patterns, making them valuable in the field of optics. Scientists have harnessed these properties for various technological applications, including the development of advanced materials for electronics and photonics.In addition to their scientific significance, anorthic (无对称的) minerals also hold aesthetic value. Many gemstones exhibit anorthic (无对称的) characteristics, which contribute to their allure and uniqueness. Collectors and jewelers often seek out these minerals for their distinctive appearances, which can vary dramatically depending on their crystalline structure.Moreover, the study of anorthic (无对称的) minerals can provide insights into the environmental conditions present during their formation. By analyzing the chemical composition and structural properties of these minerals, researchers can infer the temperature, pressure, and chemical environment of the geological processes that created them. This information is invaluable for understanding not only the minerals themselves but also the broader geological context in which they exist.In conclusion, the term anorthic (无对称的) encapsulates a rich area of study within mineralogy. The unique properties of anorthic (无对称的) crystals have implications for both scientific research and practical applications. As we continue to explore the complexities of these minerals, our understanding of their role in nature and technology will undoubtedly deepen. The fascination with anorthic (无对称的) structures is a testament to the intricate beauty and complexity of the natural world.

无对称晶体的概念令人着迷，并在矿物学领域中发挥着重要作用。anorthic（无对称的）被定义为具有缺乏对称性的晶体系统，可以在各种矿物中看到，由于其结构特征而表现出独特的性质。理解anorthic（无对称的）结构的影响，帮助地质学家和材料科学家解读这些矿物的形成过程及其潜在应用。在地质学的世界中，矿物的分类至关重要。矿物根据其晶体系统进行分类，包括立方、四方、六方、正交、单斜和anorthic（无对称的）。每个系统都有不同的对称元素，定义其形状和性质。anorthic（无对称的）系统特别引人注目，因为它不具备其他晶体系统中发现的对称特征。最显著的anorthic（无对称的）矿物之一是斜长石，这是一种常见的火成岩成分。这种矿物表现出一系列的成分，并且可以显示出不同程度的anorthic（无对称的）特征。对这些矿物的研究揭示了一个地区的地质历史，包括岩石形成时的条件。此外，某些矿物的anorthic（无对称的）特性可以影响它们的物理性质，如硬度、解理和光学特性。例如，anorthic（无对称的）晶体中的对称性缺失可能导致独特的光折射模式，使其在光学领域中具有价值。科学家们利用这些特性开发用于电子学和光子学的先进材料。除了科学意义外，anorthic（无对称的）矿物还具有美学价值。许多宝石展现出anorthic（无对称的）特性，这使它们更具吸引力和独特性。收藏家和珠宝商通常寻求这些矿物，以其独特的外观而著称，这些外观可能因其晶体结构而大相径庭。此外，对anorthic（无对称的）矿物的研究可以提供有关其形成期间环境条件的见解。通过分析这些矿物的化学成分和结构特性，研究人员可以推断出形成它们的地质过程的温度、压力和化学环境。这些信息对于理解不仅是矿物本身，而且是它们存在的更广泛的地质背景至关重要。总之，术语anorthic（无对称的）涵盖了矿物学中的一个丰富研究领域。anorthic（无对称的）晶体的独特性质对科学研究和实际应用都有影响。随着我们继续探索这些矿物的复杂性，我们对它们在自然和技术中角色的理解无疑会加深。对anorthic（无对称的）结构的迷恋证明了自然界的复杂美丽。