epidote

简明释义

英[ˈepɪdəʊt]美[ˈepəˌdoʊt]

n. [矿物] 绿帘石

英英释义

单词用法

同义词

反义词

例句

1.The characteristics of three metamorphic stages are as follows: before the eclogite-facies stage which is middle-pressure epidote amphibolite facies;

三个变质作用阶段的特征是：前榴辉相阶段为中压相系绿帘角闪岩相；

2.The characteristics of three metamorphic stages are as follows: before the eclogite-facies stage which is middle-pressure epidote amphibolite facies;

三个变质作用阶段的特征是：前榴辉相阶段为中压相系绿帘角闪岩相；

3.Mineralogically, zoisite is a member of the epidote group, the other members of which are clinozoisite, epidote perse, piemontite, and allanite.

从矿物学上讲，黝帘石是绿帘石家族的一员，绿帘石还有褐帘石等。

4.Epidote-tremolite jade called "Qinghua jade"by sellers is a new species in the market, and its main colour is blackish green or yellowish green.

绿帘石透闪石玉是市场上发现的一新品种，主体呈特征的黑绿色和黄绿色，商家称其为“青花玉”。

5.The processing flowsheet of "epidote removal by magnetic separation-calcite and quartz removal by flotation" is selected.

选择了磁选除绿帘石、浮选脱除方解石和石英的合理工艺流程。

6.The eclogites are composed of garnet, phengite, epidote, quartz, rutile, etc.

榴辉岩由石榴子石、多硅白云母、绿帘石、石英、金红石等组成。

7.As a result, the eclogite was transformed to epidote-bearing amphibolite.

榴辉岩转化成含帘石的斜长角闪岩。

8.Mineralogically, zoisite is a member of the epidote group, the other members of which are clinozoisite and allanite.

从矿物学上讲，黝帘石是绿帘石家族的一员，其他成员还有斜硅沸石和尿囊石。

9.The rock sample contained a significant amount of epidote, which is known for its distinctive green color.

这块岩石样本中含有大量的绿泥石，它以其独特的绿色而闻名。

10.Geologists often study epidote 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。

11.In mineral collections, epidote is prized for its unique crystal formations.

在矿物收藏中，绿泥石因其独特的晶体形态而受到珍视。

12.The presence of epidote can indicate high-grade metamorphic rocks.

存在绿泥石可能表明高等级的变质岩。

13.Some jewelry makers use epidote as a decorative stone due to its vibrant hue.

一些珠宝制造商使用绿泥石作为装饰石，因为它色彩鲜艳。

作文

Epidote is a fascinating mineral that often captures the attention of geologists and mineral enthusiasts alike. Known for its distinctive green color and unique crystal structure, epidote (绿泥石) is a member of the sorosilicate group of minerals. It typically forms in metamorphic rocks, particularly in regions that have experienced significant geological changes due to heat and pressure. The formation of epidote (绿泥石) is often associated with the alteration of plagioclase feldspar, which can lead to the development of this striking mineral. One of the most interesting aspects of epidote (绿泥石) is its role in understanding the geological history of an area. Geologists often study the presence and characteristics of epidote (绿泥石) to gain insights into the metamorphic processes that have shaped the Earth's crust. This mineral can provide valuable information about the temperature and pressure conditions during its formation, making it a key indicator in metamorphic petrology. In addition to its scientific significance, epidote (绿泥石) is also appreciated for its aesthetic qualities. The vibrant green hues of epidote (绿泥石) make it a popular choice among collectors and jewelry makers. Its unique crystal formations can create stunning decorative pieces, adding a touch of natural beauty to any collection. Many people are drawn to epidote (绿泥石) not only for its visual appeal but also for its purported metaphysical properties. Some believe that epidote (绿泥石) can promote positive energy and personal growth, making it a sought-after stone for those interested in healing and spiritual practices. The study of epidote (绿泥石) extends beyond just its physical characteristics; it also encompasses its chemical composition. epidote (绿泥石) is primarily composed of calcium, aluminum, iron, and silicon, which contribute to its distinct properties. The presence of different elements can lead to variations in color and appearance, making each specimen unique. This diversity is one of the reasons why epidote (绿泥石) is so highly valued by mineral collectors. Overall, epidote (绿泥石) is a remarkable mineral that holds both scientific and aesthetic value. Its ability to provide insights into the Earth's geological history, combined with its striking appearance, makes it a subject of interest for many. Whether you are a geologist studying the complexities of metamorphic rocks or a collector admiring the beauty of nature's creations, epidote (绿泥石) offers a unique glimpse into the wonders of the natural world. As we continue to explore and understand minerals like epidote (绿泥石), we gain a deeper appreciation for the intricate processes that shape our planet and the beautiful materials it produces.

绿泥石是一种迷人的矿物，常常吸引地质学家和矿物爱好者的注意。以其独特的绿色和独特的晶体结构而闻名，epidote（绿泥石）是硅酸盐矿物族的一员。它通常形成于变质岩中，特别是在经历了由于热和压力而发生显著地质变化的地区。epidote（绿泥石）的形成通常与斜长石的改变有关，这可以导致这种引人注目的矿物的发展。 epidote（绿泥石）最有趣的方面之一是它在理解一个地区的地质历史中的作用。地质学家经常研究epidote（绿泥石）的存在和特征，以获得关于塑造地壳的变质过程的见解。这种矿物可以提供关于其形成期间温度和压力条件的宝贵信息，使其成为变质岩石学中的关键指标。 除了科学意义，epidote（绿泥石）还因其美学品质而受到欣赏。epidote（绿泥石）鲜艳的绿色使其成为收藏家和珠宝制造商的热门选择。其独特的晶体形态可以创造出令人惊叹的装饰品，为任何收藏增添自然之美。许多人不仅被epidote（绿泥石）的视觉吸引，还被其声称的心灵属性所吸引。一些人相信epidote（绿泥石）可以促进积极的能量和个人成长，使其成为那些对疗愈和精神实践感兴趣的人的追捧之物。 对epidote（绿泥石）的研究不仅限于其物理特性；它还包括其化学成分。epidote（绿泥石）主要由钙、铝、铁和硅组成，这些元素对其独特的性质起着重要作用。不同元素的存在可以导致颜色和外观的变化，使每个标本都独一无二。这种多样性是epidote（绿泥石）如此受到矿物收藏家的高度重视的原因之一。 总的来说，epidote（绿泥石）是一种显著的矿物，具有科学和美学价值。它能够提供关于地球地质历史的见解，加上其引人注目的外观，使其成为许多人的兴趣对象。无论你是研究变质岩复杂性的地质学家，还是欣赏自然创造之美的收藏家，epidote（绿泥石）都为我们提供了一个独特的视角，让我们领略自然界的奇迹。随着我们继续探索和理解像epidote（绿泥石）这样的矿物，我们对塑造我们星球的复杂过程及其产生的美丽材料的欣赏也会加深。