aluminum epidote

简明释义

斜黝帘石;

英英释义

例句

1.During the field trip, students were excited to collect samples of aluminum epidote from the local quarry.

在实地考察中，学生们兴奋地从当地采石场收集铝绿泥石样本。

2.The mineral collector proudly displayed his rare specimen of aluminum epidote at the exhibition.

这位矿物收藏家在展览会上自豪地展示了他的稀有铝绿泥石标本。

3.The jewelry designer incorporated aluminum epidote into her latest collection, showcasing its unique green hues.

这位珠宝设计师在她的最新系列中融入了铝绿泥石，展示了其独特的绿色色调。

4.In the laboratory, researchers analyzed the properties of aluminum epidote to understand its potential industrial applications.

在实验室中，研究人员分析了铝绿泥石的性质，以了解其潜在的工业应用。

5.The geologist found a sample of aluminum epidote in the mountainous region, which is known for its rich mineral deposits.

地质学家在山区发现了一块铝绿泥石样本，该地区以其丰富的矿物储量而闻名。

作文

Aluminum epidote, a mineral that belongs to the epidote group, is composed primarily of aluminum, silicon, and oxygen. This fascinating mineral has garnered attention not only for its unique chemical composition but also for its striking appearance and significant geological implications. Understanding aluminum epidote (铝绿泥石) provides insights into various geological processes and the formation of metamorphic rocks.Epidote minerals are typically characterized by their greenish-yellow color and elongated crystal structure. The presence of aluminum within its structure contributes to the mineral's stability and its ability to form under specific conditions of temperature and pressure. When studying aluminum epidote (铝绿泥石), geologists often focus on its role in metamorphic environments where it can indicate the presence of certain parent rocks and the conditions under which they were altered.One of the most intriguing aspects of aluminum epidote (铝绿泥石) is its occurrence in various geological settings. It is commonly found in high-grade metamorphic rocks such as schists and gneisses, where it forms during the metamorphism of igneous and sedimentary rocks. The formation of aluminum epidote (铝绿泥石) is often associated with the alteration of plagioclase feldspar, which releases aluminum that subsequently combines with other elements to create this unique mineral.In addition to its geological significance, aluminum epidote (铝绿泥石) is also of interest to collectors and mineral enthusiasts due to its aesthetic qualities. The mineral can exhibit a vitreous luster, making it an appealing specimen for display. Its crystal formations can range from small, intricate clusters to larger, more robust specimens, each showcasing the mineral's unique characteristics.Furthermore, aluminum epidote (铝绿泥石) plays a vital role in understanding the history of the Earth's crust. By studying the conditions under which this mineral forms, scientists can gain valuable information about past tectonic activities and the evolution of the planet's surface. This knowledge is crucial for reconstructing geological histories and understanding the processes that shape our world.In conclusion, aluminum epidote (铝绿泥石) is much more than just a mineral; it is a key to unlocking the mysteries of geological processes and the history of our planet. Its unique composition, aesthetic appeal, and significant role in metamorphic geology make it a subject of interest for both scientists and collectors alike. As we continue to explore and study aluminum epidote (铝绿泥石), we deepen our understanding of the dynamic processes that have shaped the Earth over millions of years.

铝绿泥石是一种属于绿泥石组的矿物，主要由铝、硅和氧组成。这种迷人的矿物因其独特的化学成分以及显著的外观和重要的地质意义而受到关注。理解铝绿泥石（aluminum epidote）提供了对各种地质过程和变质岩形成的深入见解。绿泥石矿物通常以其黄绿色和细长的晶体结构为特征。铝在其结构中的存在有助于矿物的稳定性及其在特定温度和压力条件下的形成。当研究铝绿泥石（aluminum epidote）时，地质学家通常关注其在高等级变质岩石（如片岩和麻粒岩）中的作用，这些岩石在火成岩和沉积岩的变质过程中会出现铝绿泥石。铝绿泥石（aluminum epidote）的形成通常与钠长石的变质有关，释放出的铝与其他元素结合，从而形成这种独特的矿物。除了其地质意义外，铝绿泥石（aluminum epidote）还因其美学品质而引起收藏家和矿物爱好者的兴趣。这种矿物可以表现出玻璃光泽，使其成为展示的吸引标本。它的晶体形态可以从小而复杂的簇状到更大、更坚固的标本，各自展示出矿物的独特特征。此外，铝绿泥石（aluminum epidote）在理解地壳历史方面也发挥着重要作用。通过研究这种矿物形成的条件，科学家可以获得有关过去构造活动和地球表面演变的宝贵信息。这些知识对于重建地质历史和理解塑造我们世界的过程至关重要。总之，铝绿泥石（aluminum epidote）不仅仅是一种矿物；它是解锁地质过程和我们星球历史之谜的关键。其独特的成分、美学吸引力以及在变质地质中的重要角色使其成为科学家和收藏家共同感兴趣的对象。随着我们继续探索和研究铝绿泥石（aluminum epidote），我们加深了对数百万年来塑造地球的动态过程的理解。