basalt melts

简明释义

玄武岩质熔岩;

英英释义

Basalt melts refer to the process where basalt rock, a common volcanic rock, is heated to a temperature at which it transitions from a solid state to a liquid state.

玄武岩熔化是指玄武岩这种常见的火山岩在加热到一定温度后,从固态转变为液态的过程。

例句

1.In volcanic eruptions, basalt melts 玄武岩熔化 and can flow out to create new landforms.

在火山爆发中,basalt melts 玄武岩熔化 并可以流出形成新的地貌。

2.The process by which basalt melts 玄武岩熔化 is crucial for understanding plate tectonics.

了解 basalt melts 玄武岩熔化 的过程对于理解板块构造至关重要。

3.Geologists study how basalt melts 玄武岩熔化 under pressure to understand magma formation.

地质学家研究如何在压力下 basalt melts 玄武岩熔化 以了解岩浆形成。

4.When rocks are heated deep within the Earth, basalt melts 玄武岩熔化 to form magma chambers.

当岩石在地球深处被加热时,basalt melts 玄武岩熔化 形成岩浆房。

5.When the temperature reaches over 1000 degrees Celsius, basalt melts 玄武岩熔化 and forms lava.

当温度超过1000摄氏度时,basalt melts 玄武岩熔化 并形成熔岩。

作文

Basalt is one of the most common types of volcanic rock found on Earth. It forms from the rapid cooling of basaltic lava exposed at or very near the surface of a planet or moon. The process of how basalt is created involves various geological phenomena, including the melting of pre-existing rocks under extreme heat and pressure. When we talk about how 'basalt melts' 玄武岩熔化, we are referring to this crucial stage in the rock cycle where solid rocks transform into molten material due to intense geothermal conditions. This melting can occur in various geological settings, such as at mid-ocean ridges, subduction zones, and hotspots.The significance of understanding how 'basalt melts' 玄武岩熔化 lies in its implications for volcanic activity and the formation of new landforms. For instance, when basalt melts, it can lead to the formation of magma, which is the molten rock beneath the Earth's surface. As this magma rises, it can cause volcanic eruptions. These eruptions can create new islands, mountains, and other geological features that shape our planet's landscape.Moreover, the study of 'basalt melts' 玄武岩熔化 is also essential for understanding the composition of the Earth’s mantle. The mantle is predominantly made up of peridotite, but when subjected to high temperatures and pressures, parts of it can partially melt to form basaltic magma. This process is vital for the recycling of materials within the Earth, contributing to the dynamic nature of our planet.In addition to geological processes, the concept of 'basalt melts' 玄武岩熔化 has practical applications in various fields. For example, in the construction industry, basalt fibers are increasingly being used due to their strength and durability. Understanding the melting properties of basalt helps engineers and architects design better materials that can withstand high temperatures and stress.Furthermore, the melting of basalt plays a crucial role in the field of planetary science. By studying the conditions under which 'basalt melts' 玄武岩熔化, scientists can gain insights into the geological history of other celestial bodies, such as the Moon and Mars. For instance, the presence of basaltic rocks on the Moon suggests that volcanic activity occurred there in the past, providing clues about its thermal evolution.In conclusion, the phenomenon of how 'basalt melts' 玄武岩熔化 is not just a simple geological process; it is a fundamental aspect of our Earth’s geology and has far-reaching implications across various scientific disciplines. From understanding volcanic eruptions to exploring the composition of other planets, the melting of basalt serves as a key to unlocking many mysteries of the natural world. Therefore, continued research into this area is essential for both academic inquiry and practical applications in technology and engineering.

玄武岩是地球上最常见的一种火山岩。它由暴露在地表或非常接近地表的玄武岩熔岩迅速冷却而形成。玄武岩的形成过程涉及多种地质现象,包括在极端高温和压力下,已有岩石的熔化。当我们谈论“玄武岩熔化”时,我们指的是岩石循环中这个关键阶段,在这个阶段,固体岩石由于强烈的地热条件转变为熔融物质。这种熔化可以在各种地质环境中发生,例如中洋脊、俯冲带和热点。理解“玄武岩熔化”的重要性在于它对火山活动和新地貌形成的影响。例如,当玄武岩熔化时,它可以导致岩浆的形成,而岩浆是地球表面下的熔融岩石。当这种岩浆上升时,它可能导致火山喷发。这些喷发可以创造新的岛屿、山脉以及塑造我们星球地貌的其他地质特征。此外,研究“玄武岩熔化”对理解地球地幔的组成也至关重要。地幔主要由橄榄岩组成,但当其受到高温和高压时,部分区域可以部分熔化形成玄武岩岩浆。这一过程对地球内部物质的循环至关重要,促进了我们星球动态特性的形成。除了地质过程外,“玄武岩熔化”的概念在多个领域也有实际应用。例如,在建筑行业,由于其强度和耐用性,玄武岩纤维越来越多地被使用。了解玄武岩的熔化特性帮助工程师和建筑师设计出能承受高温和压力的更好材料。此外,玄武岩的熔化在行星科学领域也发挥着关键作用。通过研究“玄武岩熔化”的条件,科学家可以深入了解其他天体的地质历史,例如月球和火星。例如,月球上存在的玄武岩岩石表明,过去那里发生过火山活动,为其热演化提供了线索。总之,“玄武岩熔化”现象不仅仅是一个简单的地质过程;它是我们地球地质的基本方面,并在多个科学学科中具有深远的影响。从理解火山喷发到探索其他行星的组成,玄武岩的熔化是揭开自然世界许多奥秘的关键。因此,继续在这一领域进行研究对于学术探讨和技术与工程的实际应用都是至关重要的。

相关单词

basalt

basalt详解:怎么读、什么意思、用法

melts

melts详解:怎么读、什么意思、用法