marialite
简明释义
英[ˈmɛəriəˌlaɪt]美[ˈmɛəriəˌlaɪt]
n. [矿物] 钠柱石
英英释义
Marialite is a mineral belonging to the feldspar group, characterized by its sodium-rich composition and typically found in volcanic rocks. | 马里亚石是一种属于长石矿物组的矿物,以其富含钠的成分为特征,通常在火山岩中发现。 |
单词用法
同义词
锂辉石 | 玛利亚石常见于火山岩中。 |
反义词
磷灰石 | 磷灰石常见于火成岩和变质岩中。 | ||
长石 | 长石是地壳中最丰富的矿物。 |
例句
1.The sole gem marialite deposit in China is located at the western foot of Mount Muztagh, Akto County, Xinjiang, which is tectonically belongs to the Central Famirs fold belt.
中国已知的宝石级钠柱石矿床仅有一处,位于新疆阿克陶县苏巴什达坂北其依达克附近。
2.The sole gem marialite deposit in China is located at the western foot of Mount Muztagh, Akto County, Xinjiang, which is tectonically belongs to the Central Famirs fold belt.
中国已知的宝石级钠柱石矿床仅有一处,位于新疆阿克陶县苏巴什达坂北其依达克附近。
3.The presence of marialite in the rock indicates a volcanic origin.
岩石中存在marialite表明其火山起源。
4.The mineral sample contained a significant amount of marialite, which is known for its unique crystal structure.
这个矿物样本含有大量的marialite,它以其独特的晶体结构而闻名。
5.During the field trip, we discovered a large deposit of marialite near the old quarry.
在野外考察中,我们在旧采石场附近发现了大量的marialite沉积。
6.Geologists often study marialite to understand the conditions under which it forms.
地质学家经常研究marialite以了解它形成的条件。
7.In some regions, marialite can be found alongside other zeolite minerals.
在某些地区,marialite可以与其他沸石矿物共存。
作文
In the world of geology and mineralogy, there exists a fascinating mineral known as marialite. This mineral is a member of the feldspathoid group and is primarily composed of sodium and aluminum silicate. Its chemical formula can be represented as Na4Al3Si9O24Cl. The unique composition of marialite gives it distinct properties that make it an interesting subject of study for geologists and mineral enthusiasts alike. Found predominantly in volcanic rocks, marialite typically forms in environments where sodium-rich conditions prevail. This mineral often appears in a variety of colors, including white, gray, and even shades of blue, which can add to its aesthetic appeal. One of the most notable characteristics of marialite is its crystalline structure. The crystals can form in a range of shapes, from prismatic to tabular, and they often exhibit perfect cleavage, making them easy to identify. The presence of marialite in geological formations can provide valuable insights into the conditions under which these rocks were formed. For instance, the occurrence of marialite in a volcanic rock can indicate that the magma from which the rock originated was rich in sodium. This information can help geologists understand the evolution of volcanic systems and the processes that lead to the formation of different types of igneous rocks. Additionally, marialite has practical applications in various industries. Due to its unique properties, it is sometimes used as a flux in ceramics and glass production. The addition of marialite can lower the melting point of raw materials, making the manufacturing process more efficient. Furthermore, marialite is also studied for its potential use in the field of environmental science. Researchers are exploring the possibility of using this mineral in the remediation of contaminated soils and waters, as it may have the ability to absorb certain pollutants. Overall, the study of marialite not only contributes to our understanding of mineralogy but also has implications for various scientific and industrial fields. As we continue to explore the Earth's resources, minerals like marialite remind us of the intricate relationships between geological processes and human activities. Understanding such minerals can lead to advancements in technology, environmental conservation, and a deeper appreciation of the natural world. In conclusion, marialite is more than just a mineral; it is a key to unlocking the secrets of our planet's geological history and its future applications in science and industry. Whether you are a student, a professional geologist, or simply an enthusiast, the study of marialite offers a glimpse into the beauty and complexity of the Earth’s materials.
在地质学和矿物学的世界中,存在一种迷人的矿物,称为marialite。这种矿物是长石类矿物的一员,主要由钠和铝硅酸盐组成。其化学式可以表示为Na4Al3Si9O24Cl。marialite的独特成分赋予了它显著的特性,使其成为地质学家和矿物爱好者研究的有趣主题。marialite主要在火山岩中发现,通常形成于钠丰富的环境中。这种矿物往往呈现出多种颜色,包括白色、灰色,甚至蓝色,这增加了它的美学吸引力。marialite最显著的特点之一是其晶体结构。晶体可以形成多种形状,从棱柱形到板状,并且通常表现出完美的解理,使其易于识别。在地质构造中发现marialite可以提供有关这些岩石形成条件的宝贵见解。例如,火山岩中出现marialite可能表明,形成该岩石的岩浆富含钠。这些信息可以帮助地质学家理解火山系统的演变及导致不同类型的火成岩形成的过程。此外,marialite在各个行业中也有实际应用。由于其独特的属性,它有时被用作陶瓷和玻璃生产中的助熔剂。添加marialite可以降低原材料的熔点,使制造过程更高效。此外,研究人员还在探索marialite在环境科学领域的潜在应用。研究者们正在研究利用这种矿物来修复受污染的土壤和水体的可能性,因为它可能具有吸附某些污染物的能力。总体而言,marialite的研究不仅有助于我们理解矿物学,还有助于各种科学和工业领域的应用。随着我们继续探索地球的资源,像marialite这样的矿物提醒我们地质过程与人类活动之间错综复杂的关系。理解这些矿物可以推动技术进步、环境保护以及对自然世界更深刻的欣赏。总之,marialite不仅仅是一种矿物;它是揭开我们星球地质历史和未来科学与工业应用秘密的钥匙。无论你是学生、专业地质学家,还是单纯的爱好者,研究marialite都能让你一窥地球材料的美丽与复杂。