chloritic
简明释义
adj. 亚氯酸盐的
英英释义
Relating to or containing chlorite, a mineral that is a part of the mica group and often found in metamorphic rocks. | 与氯化物相关或含有氯化物,这是一种矿物,属于云母组,通常在变质岩中发现。 |
单词用法
绿泥石片岩 | |
绿泥石变质 | |
绿泥石粘土 | |
绿泥石矿物 |
同义词
带绿色的 | The mineral has a chloritic appearance due to its greenish color. | 由于其绿色外观,这种矿物呈现出氯质的特征。 | |
氯的 | Chlorous compounds are often used in disinfection processes. | 氯化合物常用于消毒过程。 |
反义词
铁的 | Ferrous materials are often used in construction due to their strength. | 铁质材料由于其强度常用于建筑。 | |
镁的 | 镁质矿物对土壤肥力非常重要。 |
例句
1.In the Ranger area highly chloritic rocks were believed to be altered dolerites.
兰杰地区的强烈绿泥石化岩石据信可能是蚀变粒玄岩。
2.In the Ranger area highly chloritic rocks were believed to be altered dolerites.
兰杰地区的强烈绿泥石化岩石据信可能是蚀变粒玄岩。
3.The presence of chloritic 绿泥石的 clay in the soil indicates good moisture retention.
土壤中存在的chloritic 绿泥石的 粘土表明良好的水分保持能力。
4.The geologist identified the rock as containing significant amounts of chloritic 绿泥石的 minerals.
地质学家确认这块岩石含有大量的chloritic 绿泥石的 矿物。
5.The chloritic 绿泥石的 alteration of the rock suggests a history of hydrothermal activity.
岩石的chloritic 绿泥石的 变质表明有热液活动的历史。
6.Geochemical analysis revealed that the mineral deposit was rich in chloritic 绿泥石的 compounds.
地球化学分析显示矿床富含chloritic 绿泥石的 化合物。
7.In the laboratory, we observed that the sample had a chloritic 绿泥石的 texture under the microscope.
在实验室中,我们观察到样本在显微镜下具有chloritic 绿泥石的 纹理。
作文
The study of minerals and their properties is a fascinating field that reveals much about the Earth’s composition and history. Among the various types of minerals, those classified as chloritic (含氯的) are particularly interesting due to their unique characteristics and formation processes. Chloritic minerals are typically greenish in color and are often found in metamorphic rocks, where they form under specific conditions of temperature and pressure. These minerals are important indicators of the geological environment in which they develop, and they can provide valuable insights into the history of a region.One of the most common chloritic (含氯的) minerals is chlorite, which is typically formed in low-grade metamorphic environments. Chlorite is known for its layered structure and can be identified by its perfect cleavage, allowing it to break easily along specific planes. This mineral often forms as a result of the alteration of other silicate minerals, such as biotite or hornblende, during the metamorphic process. The presence of chloritic (含氯的) minerals in a rock sample can indicate that the rock has undergone significant changes, providing geologists with clues about the conditions that prevailed during its formation.In addition to their geological significance, chloritic (含氯的) minerals also have practical applications. For instance, chlorite is sometimes used in the manufacture of ceramics and glass due to its heat-resistant properties. Moreover, the study of these minerals contributes to our understanding of soil formation and fertility, as they can influence the chemical composition of soils and the availability of nutrients for plants.The environmental implications of chloritic (含氯的) minerals are also noteworthy. As they weather and break down, they can release essential nutrients into the soil, promoting plant growth. However, excessive weathering of certain chloritic (含氯的) minerals can lead to the leaching of harmful elements, which may negatively impact local ecosystems. Therefore, understanding the behavior of chloritic (含氯的) minerals is crucial for managing natural resources and protecting the environment.In conclusion, chloritic (含氯的) minerals play a vital role in geology, ecology, and various industrial applications. Their unique properties not only help scientists decipher the Earth’s geological history but also contribute to practical solutions in agriculture and environmental management. As we continue to explore and learn about these minerals, we gain a deeper appreciation for the complex interactions within our planet’s systems. The study of chloritic (含氯的) minerals exemplifies how even the smallest components of the Earth can have significant impacts on both the environment and human activities.
矿物及其性质的研究是一个引人入胜的领域,揭示了地球的成分和历史。在各种类型的矿物中,被归类为chloritic(含氯的)的矿物因其独特的特征和形成过程而特别有趣。Chloritic矿物通常呈绿色,通常在变质岩中发现,在特定的温度和压力条件下形成。这些矿物是它们发展所处地质环境的重要指示剂,可以为一个地区的历史提供宝贵的见解。最常见的chloritic(含氯的)矿物之一是绿泥石,它通常在低级变质环境中形成。绿泥石以其层状结构而闻名,并且可以通过其完美的解理特征来识别,这使得它能够沿特定的平面轻易断裂。这种矿物通常是由于其他硅酸盐矿物(如黑云母或角闪石)在变质过程中发生改变而形成的。岩石样品中存在chloritic(含氯的)矿物可以表明该岩石经历了显著的变化,为地质学家提供了关于其形成时所处条件的线索。除了地质意义外,chloritic(含氯的)矿物还有实际应用。例如,绿泥石有时用于制造陶瓷和玻璃,因为它具有耐热性能。此外,对这些矿物的研究有助于我们理解土壤的形成和肥力,因为它们可以影响土壤的化学成分以及植物养分的可用性。Chloritic(含氯的)矿物的环境影响也值得注意。随着它们的风化和分解,它们可以将必需的养分释放到土壤中,促进植物生长。然而,某些chloritic(含氯的)矿物的过度风化可能导致有害元素的淋洗,从而对当地生态系统产生负面影响。因此,了解chloritic(含氯的)矿物的行为对管理自然资源和保护环境至关重要。总之,chloritic(含氯的)矿物在地质学、生态学和各种工业应用中发挥着重要作用。它们独特的性质不仅帮助科学家解读地球的地质历史,还为农业和环境管理中的实际解决方案做出了贡献。随着我们继续探索和学习这些矿物,我们对地球系统内复杂相互作用的更深层次的认识也在不断加深。对chloritic(含氯的)矿物的研究体现了即使是地球上最小的组成部分也可能对环境和人类活动产生重大影响。