buried igneous intrusion

简明释义

深部火成侵入;

英英释义

例句

1.The presence of a buried igneous intrusion 埋藏的火成岩侵入体 can indicate past geological events.

一个埋藏的火成岩侵入体的存在可能表明过去的地质事件。

2.The buried igneous intrusion 埋藏的火成岩侵入体 was dated using radiometric techniques.

利用放射性测年技术对这个埋藏的火成岩侵入体进行了年代测定。

3.Studying the buried igneous intrusion 埋藏的火成岩侵入体 helped researchers understand volcanic activity in the region.

研究这个埋藏的火成岩侵入体帮助研究人员理解该地区的火山活动。

4.The geologists discovered a buried igneous intrusion 埋藏的火成岩侵入体 while drilling for oil.

地质学家在钻探石油时发现了一个埋藏的火成岩侵入体。

5.Geophysical surveys revealed the location of the buried igneous intrusion 埋藏的火成岩侵入体 beneath the sediment layers.

地球物理勘测揭示了沉积层下方的埋藏的火成岩侵入体的位置。

作文

The study of geology encompasses a vast array of topics, one of which is the formation and characteristics of igneous rocks. Among the various geological phenomena, buried igneous intrusion plays a crucial role in understanding the Earth's crust and its evolution over millions of years. To grasp the significance of buried igneous intrusion (埋藏的火成岩侵入), it is essential to first comprehend what igneous intrusions are. These formations occur when molten rock, or magma, rises from the Earth's mantle and solidifies beneath the surface. Unlike volcanic eruptions that release lava onto the surface, intrusions remain hidden, often leading to complex geological formations that can be studied through various scientific techniques.Buried igneous intrusions can vary significantly in size and shape. Some may extend over large areas, while others might be relatively small and localized. Their shapes can range from tabular to irregular, depending on the pressure and temperature conditions during their formation. The study of these formations provides valuable insights into the processes that shape our planet. For instance, analyzing the mineral composition of a buried igneous intrusion (埋藏的火成岩侵入) can reveal information about the conditions under which the magma crystallized, including the temperature and pressure at which it was formed.Moreover, buried igneous intrusions are often associated with significant geological events, such as mountain-building processes or the formation of mineral deposits. For example, many economically important minerals, including copper, gold, and nickel, are found in association with these intrusions. Understanding the relationship between buried igneous intrusion (埋藏的火成岩侵入) and mineral deposits is vital for exploration and mining industries, as it can guide geologists in locating new resources.The process of erosion also plays a significant role in exposing buried igneous intrusions. Over time, the layers of sedimentary rock above these intrusions may wear away, revealing the once-hidden formations. This exposure allows geologists to study the physical and chemical properties of the intrusions, further enhancing our understanding of their formation and the geological history of the area. Additionally, the study of these intrusions contributes to our knowledge of tectonic activity and the movement of the Earth's plates.In conclusion, buried igneous intrusion (埋藏的火成岩侵入) represents a fascinating aspect of geological study that holds key insights into the Earth's processes and history. As scientists continue to explore these formations, they unlock the mysteries of our planet's past, providing a clearer picture of how it has evolved over time. The importance of understanding these geological features cannot be overstated, as they play a pivotal role in both academic research and practical applications in resource management and environmental studies.

地质学的研究涵盖了广泛的主题，其中之一是火成岩的形成和特征。在各种地质现象中，埋藏的火成岩侵入 在理解地壳及其数百万年来的演变方面发挥着重要作用。要理解埋藏的火成岩侵入的意义（buried igneous intrusion），首先必须理解火成岩侵入是什么。这些构造发生在熔融岩石或岩浆从地幔上升并在地表下固化时。与将熔岩释放到地表的火山喷发不同，侵入物保持隐藏，通常导致复杂的地质构造，可以通过各种科学技术进行研究。埋藏的火成岩侵入的大小和形状可以有显著差异。有些可能覆盖大面积，而其他一些可能相对较小且局部化。它们的形状可以从平坦状到不规则状，具体取决于形成过程中的压力和温度条件。对这些构造的研究提供了对塑造我们星球的过程的宝贵见解。例如，分析埋藏的火成岩侵入的矿物组成可以揭示岩浆结晶时的条件，包括形成时的温度和压力。此外，埋藏的火成岩侵入通常与重大地质事件相关，例如造山过程或矿床的形成。例如，许多经济上重要的矿物，包括铜、金和镍，都是与这些侵入物相关联的。了解埋藏的火成岩侵入与矿床之间的关系对于勘探和采矿行业至关重要，因为它可以指导地质学家寻找新的资源。侵蚀过程在暴露埋藏的火成岩侵入方面也发挥了重要作用。随着时间的推移，上方沉积岩层可能会磨损，揭示出曾经隐藏的构造。这种暴露使地质学家能够研究这些侵入物的物理和化学性质，进一步增强我们对其形成及该地区地质历史的理解。此外，对这些侵入物的研究有助于我们了解构造活动和地球板块的运动。总之，埋藏的火成岩侵入（buried igneous intrusion）代表了地质研究的一个迷人方面，蕴含着对地球过程和历史的关键见解。随着科学家继续探索这些构造，他们揭开了我们星球过去的神秘，为我们提供了更清晰的图景，了解它是如何随着时间演变的。理解这些地质特征的重要性不容小觑，因为它们在学术研究和资源管理及环境研究的实际应用中都发挥着关键作用。