serpentinize

简明释义

英[ˌsɜr.pənˈtaɪz]美[ˌsɜr.pənˈtaɪz]

vi. <文>（以蛇的方式）缠绕或扭曲

vt. （矿物学）使蛇纹石化

第 三 人 称 单 数 s e r p e n t i n i z e s

现 在 分 词 s e r p e n t i n i z i n g

过 去 式 s e r p e n t i n i z e d

过 去 分 词 s e r p e n t i n i z e d

英英释义

单词用法

同义词

反义词

例句

1.The geological study revealed that the rock had undergone a process to serpentinize 蛇纹石化, transforming it into a softer mineral.

地质研究显示，这块岩石经历了一个过程，蛇纹石化 serpentinize，使其转变为一种较软的矿物。

2.In the lab, scientists observed how certain conditions could cause olivine to serpentinize 蛇纹石化 in a matter of weeks.

在实验室中，科学家观察到某些条件如何导致橄榄石在几周内蛇纹石化 serpentinize。

3.The process of serpentinize 蛇纹石化 can lead to the formation of hydrogen gas, which may have implications for microbial life.

蛇纹石化 serpentinize 的过程可能导致氢气的形成，这可能对微生物生命有影响。

4.The presence of water is crucial for the rocks to serpentinize 蛇纹石化 effectively during metamorphism.

水的存在对于岩石在变质作用中有效地蛇纹石化 serpentinize 是至关重要的。

5.Researchers are studying how the ability of mantle rocks to serpentinize 蛇纹石化 can influence tectonic activity.

研究人员正在研究地幔岩石蛇纹石化 serpentinize 的能力如何影响构造活动。

作文

The process of rock formation is a fascinating subject that reveals the dynamic nature of our planet. One of the intriguing processes involved in this transformation is known as serpentinize, which refers to the alteration of olivine and other magnesium-rich silicate minerals into serpentine minerals under conditions of high temperature and pressure. This geological phenomenon not only plays a crucial role in the formation of certain types of rocks but also has significant implications for our understanding of the Earth's mantle and tectonic activity.When we talk about serpentinize rocks, we are often referring to ultramafic rocks, which are primarily composed of olivine and pyroxene. These rocks are typically found in ophiolite complexes and are believed to originate from the Earth's mantle. The process of serpentinize occurs when these rocks are subjected to hydrothermal fluids, which can facilitate the chemical reactions necessary for the transformation into serpentine minerals. This transformation is not just a simple change in mineralogy; it involves complex physical and chemical processes that can affect the overall properties of the rock.One of the most interesting aspects of serpentinize is its association with the release of hydrogen gas, which can have profound implications for both geology and biology. The reaction that leads to serpentinize produces hydrogen as a byproduct, which can serve as an energy source for microbial life in extreme environments, such as those found in deep-sea hydrothermal vents. This discovery has led scientists to speculate about the potential for life on other planets, particularly on celestial bodies like Europa or Enceladus, where similar conditions might exist.Moreover, the study of serpentinize processes is essential for understanding the carbon cycle and the role of ultramafic rocks in sequestering carbon dioxide. As these rocks undergo serpentinize, they can absorb CO2 from the atmosphere, effectively acting as a natural carbon sink. This has significant implications for climate change, as enhancing the serpentinize process could potentially be a strategy for mitigating greenhouse gas emissions.In addition to its geological significance, serpentinize has practical applications in various industries. For instance, the serpentine minerals produced during this process are often used in the production of asbestos, although the health risks associated with asbestos have led to a decline in its use. Furthermore, the unique properties of serpentine minerals make them valuable in the field of ceramics and as a source of magnesium.In conclusion, the term serpentinize encompasses a wide range of geological, biological, and environmental processes that highlight the interconnectedness of Earth's systems. Understanding this process not only deepens our knowledge of geology but also opens up new avenues for research in astrobiology, climate science, and resource management. As we continue to explore the complexities of our planet, the significance of serpentinize will undoubtedly remain a vital area of study, shedding light on the intricate dance of minerals, fluids, and life itself.

岩石形成的过程是一个引人入胜的主题，揭示了我们星球的动态特性。在这一转变过程中，有一个有趣的过程被称为serpentinize，指的是在高温和高压条件下，橄榄石和其他富镁硅酸盐矿物转变为蛇纹石矿物的变化。这种地质现象不仅在某些类型岩石的形成中起着关键作用，还对我们理解地球的地幔和构造活动具有重要意义。当我们谈论serpentinize岩石时，通常是指超镁铁质岩石，这些岩石主要由橄榄石和辉石组成。这些岩石通常在洋壳复合体中发现，被认为起源于地球的地幔。serpentinize的过程发生在这些岩石受到热液流体的影响时，这些流体可以促进必要的化学反应，使其转变为蛇纹石矿物。这种转变不仅仅是矿物成分的简单变化；它涉及复杂的物理和化学过程，可以影响岩石的整体特性。serpentinize的一个最有趣的方面是它与氢气释放的关联，这对地质和生物学都有深远的影响。导致serpentinize的反应会产生氢气作为副产品，这可以作为极端环境中微生物生命的能量来源，例如那些在深海热液喷口中发现的生命。这一发现使科学家们开始推测，在其他行星上，特别是像欧罗巴或恩克拉多斯这样的天体上，类似条件可能存在，从而可能存在生命。此外，研究serpentinize过程对于理解碳循环及超镁铁质岩石在固定二氧化碳中的作用至关重要。当这些岩石经历serpentinize时，它们可以从大气中吸收CO2，有效地充当自然碳汇。这对气候变化具有重大意义，因为增强serpentinize过程可能是一种减缓温室气体排放的策略。除了其地质意义外，serpentinize在各个行业中也具有实际应用。例如，在这一过程中产生的蛇纹石矿物常用于石棉的生产，尽管与石棉相关的健康风险导致其使用减少。此外，蛇纹石矿物的独特性质使其在陶瓷领域和镁资源的开发中具有价值。总之，术语serpentinize涵盖了广泛的地质、生物和环境过程，突显了地球系统的相互联系。理解这一过程不仅加深了我们对地质学的认识，还为天体生物学、气候科学和资源管理的研究开辟了新的途径。随着我们继续探索我们星球的复杂性，serpentinize的重要性无疑将仍然是一个重要的研究领域，揭示矿物、流体和生命本身之间的复杂舞蹈。