chloritization

简明释义

英[ˌklɔːrɪtaɪˈzeɪʃən]美[ˌklɔrɪtɪˈzeʃən]

n. [化学] 亚氯酸化作用

英英释义

单词用法

同义词

反义词

例句

1.The greenish color of the palaeo-oxidized sandstones mainly results from chloritization and epidotization related to oil and gas secondary reduction processes.

古氧化绿色砂岩主要由与油-气二次还原作用有关的绿泥石化和绿帘石化造成。

2.There is a close relationship of gold mineralization to silicification, sericitization and chloritization. The potential reserves of this deposit may exceed a large size gold deposit.

硅化、绢云母化、绿泥石化流纹斑岩型金矿是本矿的主要金矿类型。

3.There is a close relationship of gold mineralization to silicification, sericitization and chloritization. The potential reserves of this deposit may exceed a large size gold deposit.

硅化、绢云母化、绿泥石化流纹斑岩型金矿是本矿的主要金矿类型。

4.The study of chloritization helps in identifying potential mineral deposits.

对氯化作用的研究有助于识别潜在的矿床。

5.The chloritization of biotite can indicate changes in the surrounding environment.

黑云母的氯化作用可以指示周围环境的变化。

6.In some regions, chloritization occurs due to the interaction of volcanic materials with water.

在某些地区，由于火山物质与水的相互作用，发生了氯化作用。

7.Geologists study chloritization to understand the alteration of minerals in hydrothermal systems.

地质学家研究氯化作用以了解热液系统中矿物的变化。

8.The process of chloritization is often observed in metamorphic rocks.

在变质岩中，通常可以观察到氯化作用的过程。

作文

In the field of geology, the term chloritization refers to a specific process involving the alteration of minerals, particularly feldspar and biotite, into chlorite, a greenish mineral that is part of the phyllosilicate group. This transformation occurs under certain conditions, typically involving hydrothermal activity or metamorphic processes. Understanding chloritization is crucial for geologists as it provides insights into the geological history of an area, including temperature and pressure conditions during rock formation.Chlorite itself is known for its layered structure and can influence the physical properties of rocks. The presence of chloritization in a rock sample may indicate that the rock has undergone significant changes due to environmental factors such as heat and fluid movement. For instance, when magma intrudes into surrounding rocks, the heat can cause the alteration of existing minerals through chloritization, leading to the formation of new minerals like chlorite.The study of chloritization is not only important for understanding the mineralogical composition of rocks but also plays a role in economic geology. Many mineral deposits, such as those containing copper and gold, are associated with areas where chloritization has occurred. By analyzing the extent of chloritization, geologists can identify potential locations for mining operations, making it a valuable tool in resource exploration.Furthermore, chloritization can affect the stability of slopes and the behavior of soil and rock in engineering projects. When assessing the stability of a slope, engineers must consider the degree of chloritization present in the rock, as it can weaken the material and increase the risk of landslides. Therefore, understanding this process is essential not only for geological studies but also for practical applications in civil engineering and construction.In summary, chloritization is a significant geological process that involves the alteration of minerals to form chlorite. Its implications reach far beyond the academic realm, influencing economic geology and engineering practices. As we continue to explore and understand the Earth's processes, the study of chloritization will remain a key area of focus for geologists and engineers alike. By recognizing the signs of chloritization in rock formations, we can glean valuable information about the past environments and conditions that shaped our planet's crust. This knowledge not only enriches our understanding of geology but also aids in responsible resource management and infrastructure development.

在地质学领域，术语chloritization指的是一种特定的过程，涉及矿物的变化，特别是长石和黑云母转变为绿泥石，这是一种属于层状硅酸盐组的绿色矿物。这种转变发生在特定条件下，通常涉及热液活动或变质过程。理解chloritization对于地质学家至关重要，因为它提供了一个地区地质历史的见解，包括岩石形成期间的温度和压力条件。绿泥石本身以其层状结构而闻名，可以影响岩石的物理特性。岩样中存在的chloritization可能表明该岩石由于环境因素（如热量和流体运动）经历了显著变化。例如，当岩浆侵入周围岩石时，热量可以通过chloritization导致现有矿物的变化，形成新的矿物，如绿泥石。对chloritization的研究不仅对于理解岩石的矿物组成很重要，还在经济地质学中发挥作用。许多矿床，例如含铜和金的矿床，与发生chloritization的区域相关。通过分析chloritization的程度，地质学家可以识别潜在的采矿作业位置，使其成为资源勘探中的宝贵工具。此外，chloritization可能会影响坡度的稳定性以及土壤和岩石在工程项目中的行为。在评估坡度的稳定性时，工程师必须考虑岩石中存在的chloritization程度，因为这可能削弱材料并增加滑坡风险。因此，理解这一过程对于地质研究和土木工程及建筑实践都至关重要。总之，chloritization是一个重要的地质过程，涉及矿物的变化形成绿泥石。其影响远远超出了学术领域，影响着经济地质学和工程实践。随着我们继续探索和理解地球的过程，chloritization的研究将继续成为地质学家和工程师关注的关键领域。通过识别岩石形成中的chloritization迹象，我们可以获取关于塑造我们星球地壳的过去环境和条件的宝贵信息。这些知识不仅丰富了我们对地质学的理解，还帮助我们在资源管理和基础设施发展中负责任地行事。