riebeckite

简明释义

英[ˈriːbɛkaɪt]美[ˈriːbɛkaɪt]

n. [矿物] 钠闪石

英英释义

单词用法

同义词

反义词

例句

1.Mineral constituents consist mainly of jadeite, aegirine - augite, magnesio - riebeckite, winchite , magnesio - hornblende , actinolite , quartz, albite, rutile and sphene.

主要组成矿物为硬玉、霓辉石、 镁纳闪石、蓝透闪石、镁角闪石、阳起石、石英、钠长石、金红石和榍石。

2.Mineral constituents consist mainly of jadeite, aegirine - augite, magnesio - riebeckite, winchite , magnesio - hornblende , actinolite , quartz, albite, rutile and sphene.

主要组成矿物为硬玉、霓辉石、 镁纳闪石、蓝透闪石、镁角闪石、阳起石、石英、钠长石、金红石和榍石。

3.Mineral constituents consist mainly of jadeite, aegirine - augite, magnesio - riebeckite, winchite, magnesio - hornblende, actinolite, quartz, albite, rutile and sphene.

主要组成矿物为硬玉、霓辉石、镁纳闪石、蓝透闪石、镁角闪石、阳起石、石英、钠长石、金红石和榍石。

4.The geologist explained that riebeckite 黑云母 is a common mineral found in certain types of granite.

地质学家解释说，riebeckite 黑云母 是某些类型花岗岩中常见的矿物。

5.In his research, he discovered a large deposit of riebeckite 黑云母 in the region's volcanic rocks.

在他的研究中，他发现该地区火山岩中有大量的riebeckite 黑云母 矿藏。

6.The presence of riebeckite 黑云母 can indicate high-temperature conditions during rock formation.

在岩石形成过程中，riebeckite 黑云母 的存在可能表明高温条件。

7.During the field trip, we collected samples of riebeckite 黑云母 for further analysis in the lab.

在实地考察中，我们收集了riebeckite 黑云母 的样本，以便在实验室进行进一步分析。

8.The mineral riebeckite 黑云母 is often used in studies related to metamorphic geology.

矿物riebeckite 黑云母 常用于与变质地质相关的研究中。

作文

Riebeckite is a fascinating mineral that belongs to the amphibole group. It is primarily composed of sodium, iron, and magnesium, making it a unique member of its family. This mineral is often found in igneous rocks, particularly in those that are rich in silica. The presence of riebeckite (里贝克石) can indicate certain geological conditions and can be an essential factor in understanding the formation of specific rock types. One notable feature of riebeckite is its striking dark blue to black color, which can be attributed to the iron content within its structure. This characteristic makes it easily identifiable in hand samples, and it often attracts the attention of mineral collectors and geologists alike. In geological terms, riebeckite is significant because it can provide insights into the conditions under which the host rock was formed. For example, its presence in a rock sample may suggest that the rock originated from a high-temperature environment, typical of certain volcanic or plutonic settings. Furthermore, riebeckite is often associated with other minerals such as quartz and feldspar, which can help geologists reconstruct the history of the rock and the processes that led to its formation. The study of riebeckite extends beyond geology; it also has implications in industrial applications. Due to its fibrous nature, riebeckite can sometimes be confused with asbestos, which raises health concerns. Asbestos is well-known for its hazardous properties, and the identification of riebeckite in certain materials requires careful analysis to ensure safety. This duality of riebeckite as both a valuable mineral for scientific study and a potential health risk highlights the importance of accurate mineral identification. In addition to its geological and industrial significance, riebeckite also holds aesthetic value. Mineral enthusiasts often seek out specimens of riebeckite for their collections due to their unique appearance. The glossy, dark surfaces of polished riebeckite can create stunning displays when combined with other minerals. Collectors appreciate not only the beauty of these specimens but also the stories they tell about the Earth's geological history. In conclusion, riebeckite (里贝克石) is more than just a mineral; it is a key to understanding the Earth's processes and a subject of interest for both scientists and collectors. Its distinctive characteristics, geological significance, and potential industrial applications make it a noteworthy topic in the field of mineralogy. As we continue to explore the complexities of our planet, minerals like riebeckite serve as reminders of the intricate connections between geology, industry, and aesthetics. Whether you are a professional geologist or a casual mineral enthusiast, the study of riebeckite offers a window into the dynamic processes that shape our world.

里贝克石是一种迷人的矿物，属于角闪石组。它主要由钠、铁和镁组成，使其成为该家族中独特的成员。这种矿物常见于火成岩，尤其是在富含二氧化硅的岩石中。里贝克石的存在可以指示某些地质条件，并且在理解特定岩石类型的形成中可能是一个重要因素。里贝克石的一个显著特征是其引人注目的深蓝色到黑色，这可以归因于其结构中的铁含量。这一特征使其在手样中易于识别，并且常常吸引矿物收藏者和地质学家的注意。 在地质学上，里贝克石是重要的，因为它可以提供关于宿主岩石形成条件的见解。例如，其在岩石样本中的存在可能表明该岩石起源于高温环境，典型于某些火山或深成环境。此外，里贝克石通常与其他矿物如石英和长石相关联，这可以帮助地质学家重建岩石的历史及导致其形成的过程。 对里贝克石的研究不仅限于地质学；它在工业应用中也有影响。由于其纤维状特性，里贝克石有时会与石棉混淆，这引发了健康问题。石棉以其危险特性而闻名，在某些材料中识别里贝克石需要仔细分析以确保安全。这种里贝克石作为科学研究的宝贵矿物与潜在健康风险的双重性突显了准确矿物识别的重要性。 除了其地质和工业意义外，里贝克石还具有美学价值。矿物爱好者常常寻求里贝克石的标本以丰富他们的收藏，因为其独特的外观。抛光后的里贝克石的光滑黑暗表面可以与其他矿物结合，创造出惊艳的展示。收藏家欣赏这些标本的美丽以及它们讲述的关于地球地质历史的故事。 总之，里贝克石不仅仅是一种矿物；它是理解地球过程的关键，也是科学家和收藏者感兴趣的主题。其独特的特征、地质重要性和潜在的工业应用使其在矿物学领域成为一个值得注意的话题。随着我们继续探索地球的复杂性，像里贝克石这样的矿物提醒我们地质、工业和美学之间的复杂联系。无论您是专业地质学家还是休闲矿物爱好者，里贝克石的研究都为我们提供了一个了解塑造我们世界的动态过程的窗口。