clinochlore

简明释义

英[ˈklaɪnəˌklɔr]美[ˈklaɪnəˌklɔr]

n. [矿物] 斜绿泥石

英英释义

单词用法

同义词

反义词

例句

1.Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉石英、斜绿泥石的晶体结构和表面性质以及油酸作阴离子捕收剂时的溶液化学。

2.Furthermore, the crystal structure, surface characters of quartz and clinochlore, and the solution chemistry of oleic acid as the anionic collector were analyzed.

分析粉石英、斜绿泥石的晶体结构和表面性质以及油酸作阴离子捕收剂时的溶液化学。

3.During the mineral identification process, we discovered a sample of clinochlore that had not been cataloged before.

在矿物鉴定过程中，我们发现了一种之前未被归档的绿泥石样本。

4.The presence of clinochlore in the rock indicates a history of high-pressure metamorphism.

岩石中存在绿泥石表明其经历了高压变质的历史。

5.The mineral sample contained significant amounts of clinochlore, which is known for its green color and layer structure.

该矿物样本含有大量的绿泥石，它以绿色和层状结构而闻名。

6.In some regions, clinochlore is used as a gemstone in jewelry due to its unique appearance.

在某些地区，绿泥石因其独特的外观而被用作珠宝中的宝石。

7.Geologists often study clinochlore to understand the metamorphic processes in the Earth's crust.

地质学家经常研究绿泥石以了解地壳中的变质过程。

作文

Clinochlore, a mineral belonging to the chlorite group, is often recognized for its distinctive green color and layered structure. This mineral is primarily composed of magnesium, iron, and aluminum silicate, which contributes to its unique properties. The name clinochlore derives from the Greek words 'klino,' meaning 'to lean,' and 'chloros,' meaning 'green,' reflecting its characteristic green hue. In geology, clinochlore is significant not only for its aesthetic appeal but also for its role in the formation of metamorphic rocks. It is commonly found in schist and other metamorphic environments, where it forms through the alteration of mica and other minerals under high-pressure and high-temperature conditions.The occurrence of clinochlore is widespread, especially in regions with a history of volcanic activity or tectonic movements. For instance, it can be found in the Alps, the Himalayas, and various locations in North America. The presence of clinochlore often indicates specific geological processes, such as the metamorphism of sedimentary rocks. Its layered structure allows it to be easily split into thin sheets, which is a characteristic feature of many chlorite minerals.In addition to its geological significance, clinochlore has applications in various industries. For example, its unique properties make it an interesting subject for research in materials science and nanotechnology. Scientists are exploring how the layered structure of clinochlore can be utilized in creating new materials with enhanced properties, such as improved strength and flexibility. Furthermore, due to its natural abundance and non-toxic nature, clinochlore is being investigated for use in environmental applications, including soil remediation and as a potential source of magnesium.The study of clinochlore also provides insights into the broader field of mineralogy and petrology. Understanding the formation and transformation of this mineral can help researchers decipher the complex histories of metamorphic rocks and the conditions under which they formed. Moreover, the examination of clinochlore can shed light on the processes that govern mineral stability and transformation, contributing to our knowledge of Earth's geological processes.In conclusion, clinochlore is more than just a visually appealing mineral; it is a key player in the geological narrative of our planet. Its unique composition, formation, and applications make it a fascinating subject for study. As we continue to explore the properties and potential uses of clinochlore, we gain a deeper appreciation for the intricate connections between minerals, geology, and the environment. Whether in the context of academic research or practical applications, clinochlore represents a bridge between the natural world and human innovation, highlighting the importance of understanding and preserving our planet's mineral resources.

克林氯石是一种属于氯矿物组的矿物，因其独特的绿色和层状结构而受到广泛认可。这种矿物主要由镁、铁和铝硅酸盐组成，这使其具有独特的性质。克林氯石这个名字源自希腊语单词“klino”，意为“倾斜”，和“chloros”，意为“绿色”，反映出其特有的绿色色调。在地质学中，克林氯石不仅因其美学吸引力而显得重要，还因其在变质岩形成中的作用而备受关注。它通常出现在片麻岩及其他变质环境中，在高压和高温条件下通过云母和其他矿物的变化而形成。克林氯石的出现非常普遍，尤其是在具有火山活动或构造运动历史的地区。例如，它可以在阿尔卑斯山、喜马拉雅山和北美的多个地点找到。克林氯石的存在往往指示着特定的地质过程，例如沉积岩的变质作用。它的层状结构使其容易分裂成薄片，这是许多氯矿物的特征。除了其地质意义外，克林氯石在各个行业都有应用。例如，其独特的性质使其成为材料科学和纳米技术研究的有趣对象。科学家们正在探索如何利用克林氯石的层状结构来创建具有增强性能的新材料，如提高强度和柔韧性。此外，由于其自然丰富和无毒的特性，克林氯石也正在被研究用于环境应用，包括土壤修复和作为潜在的镁来源。对克林氯石的研究还为矿物学和岩石学的更广泛领域提供了见解。理解这种矿物的形成和转变可以帮助研究人员解读变质岩的复杂历史以及它们形成的条件。此外，对克林氯石的研究可以阐明支配矿物稳定性和转化过程的机制，从而丰富我们对地球地质过程的认识。总之，克林氯石不仅仅是一种视觉上迷人的矿物；它是我们星球地质叙事中的关键角色。其独特的成分、形成和应用使其成为一个引人入胜的研究主题。随着我们继续探索克林氯石的性质和潜在用途，我们对矿物、地质和环境之间复杂联系的理解将更加深入。无论是在学术研究还是实际应用的背景下，克林氯石都代表了自然世界与人类创新之间的桥梁，突显了理解和保护我们星球矿产资源的重要性。