anatectic crystallization

简明释义

深溶结晶作用;

英英释义

Anatectic crystallization refers to the process of melting and subsequent crystallization of rocks, typically occurring in high-temperature conditions where partial melting leads to the formation of magma that then cools to form igneous rocks.

Anatectic crystallization指的是岩石的熔化及随后的结晶过程,通常发生在高温条件下,部分熔化导致岩浆的形成,随后冷却形成火成岩。

例句

1.The research team focused on the process of anatectic crystallization to understand how magma evolves in the Earth's crust.

研究小组专注于再熔结晶的过程,以了解地壳中岩浆如何演变。

2.During field studies, we observed signs of anatectic crystallization in several rock formations.

在野外研究中,我们观察到几个岩层中有再熔结晶的迹象。

3.The presence of anatectic crystallization is often indicated by unique mineral compositions in metamorphic rocks.

在变质岩中,再熔结晶的存在通常通过独特的矿物成分来指示。

4.Understanding anatectic crystallization helps geologists predict volcanic activity based on magma composition.

理解再熔结晶有助于地质学家根据岩浆成分预测火山活动。

5.In geology, anatectic crystallization can lead to the formation of new igneous rocks from partially melted materials.

在地质学中,再熔结晶可以导致从部分熔化的材料形成新的火成岩。

作文

In the study of geology, the term anatectic crystallization refers to a specific process that occurs during the metamorphism of rocks. This process involves the partial melting of pre-existing rocks, which leads to the formation of new mineral phases as the molten material cools and solidifies. Understanding anatectic crystallization is crucial for geologists as it helps them interpret the history and evolution of the Earth's crust. When rocks are subjected to high temperatures and pressures, they can undergo significant changes. The original minerals may begin to melt, creating a magma-like substance. This partially melted rock can then migrate and mix with surrounding materials, leading to complex geological formations. The cooling of this molten material results in the crystallization of new minerals, which can provide insights into the conditions under which the rock formed. The significance of anatectic crystallization extends beyond mere academic interest; it has practical implications in various fields. For instance, understanding this process can aid in the exploration of natural resources such as metals and gemstones. Many valuable minerals are formed through the processes associated with anatectic crystallization, making it a topic of interest for mining companies and environmental scientists alike.Moreover, the study of anatectic crystallization contributes to our knowledge of tectonic movements and plate boundaries. As tectonic plates interact, they create conditions conducive to the melting of rocks. By examining the products of anatectic crystallization, scientists can infer the dynamics of these geological processes and their impact on the Earth's surface. In addition to its geological significance, anatectic crystallization also offers a fascinating glimpse into the Earth's history. The minerals formed during this process can serve as time capsules, preserving information about the temperature and pressure conditions of their formation. By studying these minerals, geologists can reconstruct past environments and understand how the Earth has changed over millions of years. Furthermore, anatectic crystallization plays a role in the broader context of the rock cycle. This cycle describes the continuous transformation of rocks from one type to another, driven by geological processes. The melting and recrystallization associated with anatectic crystallization illustrate the dynamic nature of the Earth’s crust and highlight the interconnectedness of different geological processes. In conclusion, anatectic crystallization is a vital concept in geology that encompasses the processes of partial melting and subsequent crystallization of rocks. Its implications extend to resource exploration, tectonic studies, and our understanding of the Earth's geological history. By delving into the intricacies of anatectic crystallization, we gain valuable insights into the complex mechanisms that shape our planet and the materials that comprise it.

在地质学研究中,术语anatectic crystallization指的是一种特定的过程,该过程发生在岩石的变质作用期间。这一过程涉及到对先存岩石的部分熔融,从而在熔融材料冷却并固化时形成新的矿物相。理解anatectic crystallization对地质学家至关重要,因为它帮助他们解读地壳的历史和演化。当岩石受到高温和高压的作用时,它们可能会经历显著的变化。原始矿物可能开始熔化,产生类似于岩浆的物质。这种部分熔融的岩石可以迁移并与周围材料混合,导致复杂的地质构造。这种熔融材料的冷却导致新矿物的结晶,这可以提供关于岩石形成条件的见解。anatectic crystallization的重要性超出了学术兴趣;它在各个领域具有实际意义。例如,理解这一过程可以帮助探索自然资源,如金属和宝石。许多有价值的矿物是通过与anatectic crystallization相关的过程形成的,这使其成为采矿公司和环境科学家感兴趣的话题。此外,anatectic crystallization的研究有助于我们了解构造运动和板块边界。当构造板块相互作用时,会产生有利于岩石熔融的条件。通过检查anatectic crystallization的产物,科学家可以推断这些地质过程的动态及其对地球表面的影响。除了其地质重要性,anatectic crystallization还为我们提供了对地球历史的迷人视角。这个过程中形成的矿物可以作为时间胶囊,保存关于其形成时温度和压力条件的信息。通过研究这些矿物,地质学家可以重建过去的环境,理解地球在数百万年间的变化。此外,anatectic crystallization在岩石循环的更广泛背景中也发挥着作用。这个循环描述了岩石从一种类型转变为另一种类型的连续转化,受到地质过程的驱动。与anatectic crystallization相关的熔融和再结晶展示了地壳的动态特性,并突显了不同地质过程之间的相互联系。总之,anatectic crystallization是地质学中的一个重要概念,涵盖了岩石的部分熔融和随后的结晶过程。它的影响扩展到资源探索、构造研究以及我们对地球地质历史的理解。通过深入探讨anatectic crystallization的复杂性,我们获得了关于塑造我们星球及其组成材料的复杂机制的宝贵见解。

相关单词

crystallization

crystallization详解:怎么读、什么意思、用法