autochthonous autoclastic

简明释义

自碎的;

英英释义

例句

1.The analysis of autochthonous autoclastic 原生自碎屑岩 formations can reveal the tectonic history of an area.

对autochthonous autoclastic 原生自碎屑岩 形成的分析可以揭示一个地区的构造历史。

2.In sedimentology, autochthonous autoclastic 原生自碎屑岩 deposits are crucial for understanding local geological history.

在沉积学中，autochthonous autoclastic 原生自碎屑岩 沉积物对于理解当地地质历史至关重要。

3.The formation was primarily composed of autochthonous autoclastic 原生自碎屑岩 sediments, indicating minimal transport from their source.

该地层主要由autochthonous autoclastic 原生自碎屑岩 沉积物组成，表明其来源地的运输极小。

4.Researchers found that the autochthonous autoclastic 原生自碎屑岩 layers were rich in fossils, providing insights into ancient ecosystems.

研究人员发现，autochthonous autoclastic 原生自碎屑岩 层富含化石，为古生态系统提供了见解。

5.The geologist studied the layers of rock to identify the presence of autochthonous autoclastic 原生自碎屑岩 materials in the formation.

地质学家研究了岩层，以识别该地层中存在的autochthonous autoclastic 原生自碎屑岩 材料。

作文

The study of geology often requires a deep understanding of various terms that describe the formation and characteristics of rocks and minerals. One such term that may not be familiar to many is autochthonous autoclastic. To fully grasp its meaning, we must break it down into its components. The word 'autochthonous' originates from the Greek word 'autochthon', meaning 'native' or 'indigenous'. In geological terms, it refers to materials or formations that are formed in the same location where they are found. This is significant because it implies a direct relationship between the rock and its environment, indicating that the rock has not been transported from another location.On the other hand, 'autoclastic' comes from the combination of 'auto', meaning 'self', and 'clastic', which relates to the breaking down of rocks. Thus, autochthonous autoclastic refers to rocks or sediments that have originated from their own source material through processes such as weathering and erosion, without being displaced from their original setting. This concept is crucial for understanding sedimentary processes and the formation of certain rock types.In practical terms, identifying autochthonous autoclastic materials can provide geologists with valuable insights into the geological history of an area. For example, when examining sediment layers, geologists can determine whether the sediments were deposited locally or if they were transported from distant locations. This information can help reconstruct past environments, understand tectonic activities, and even predict future geological events.Moreover, the significance of autochthonous autoclastic formations extends beyond academic interest. They play a vital role in resource exploration, particularly in the fields of oil and gas, mining, and groundwater studies. Understanding the local geological conditions can lead to better resource management and extraction strategies.To illustrate this further, consider a river delta where sediments accumulate over time. If these sediments are identified as autochthonous autoclastic, it indicates that they were formed and deposited in situ, reflecting the current environmental conditions of the delta. Conversely, if the sediments were transported from another location, they would not be classified as such, leading to different implications regarding the delta's development and stability.In conclusion, the term autochthonous autoclastic encapsulates an important aspect of geology that emphasizes the relationship between rocks and their environments. By understanding this term, we can appreciate the complexities of geological formations and their implications for both natural processes and human activities. As we continue to explore our planet's geological features, recognizing the significance of autochthonous autoclastic materials will enhance our comprehension of the Earth's history and its dynamic systems.

地质学的研究通常需要深入理解各种术语，这些术语描述了岩石和矿物的形成及特征。其中一个可能不为许多人所熟知的术语是自生自碎。要完全掌握它的含义，我们必须将其分解成组成部分。‘自生’一词源于希腊语‘autochthon’，意为‘本土的’或‘土生土长的’。在地质学中，它指的是在发现地点形成的材料或构造。这一点非常重要，因为它暗示了岩石与其环境之间的直接关系，表明岩石没有从其他地方运输过来。另一方面，‘自碎’来自于‘自’（auto）和‘碎屑’（clastic）的结合，后者与岩石的破碎有关。因此，自生自碎指的是通过风化和侵蚀等过程，从自身源材料中产生的岩石或沉积物，而没有被移位到原始环境之外。这个概念对于理解沉积过程和某些岩石类型的形成至关重要。在实际应用中，识别自生自碎材料可以为地质学家提供有价值的见解，帮助他们了解一个地区的地质历史。例如，在检查沉积层时，地质学家可以确定沉积物是本地沉积还是从远处运输而来。这些信息可以帮助重建过去的环境，理解构造活动，甚至预测未来的地质事件。此外，自生自碎构造的重要性超出了学术兴趣。它们在资源勘探中发挥着至关重要的作用，特别是在石油和天然气、采矿和地下水研究等领域。理解当地的地质条件可以导致更好的资源管理和开采策略。为了进一步说明这一点，考虑一个河口三角洲，沉积物随着时间的推移而积累。如果这些沉积物被识别为自生自碎，这表明它们是在原地形成和沉积的，反映了三角洲当前的环境条件。相反，如果沉积物是从其他地方运输来的，它们就不会被归类为此，从而对三角洲的发展和稳定性产生不同的影响。总之，自生自碎这一术语涵盖了地质学的一个重要方面，强调了岩石与其环境之间的关系。通过理解这一术语，我们可以欣赏地质构造的复杂性及其对自然过程和人类活动的影响。随着我们继续探索地球的地质特征，认识到自生自碎材料的重要性将增强我们对地球历史及其动态系统的理解。