active source rock

简明释义

1. 有效生油岩; 2. 活性生油岩;

英英释义

例句

1.Understanding the characteristics of active source rock (活跃的源岩) is crucial for successful oil exploration.

了解活跃的源岩的特性对成功的石油勘探至关重要。

2.In this region, the active source rock (活跃的源岩) is primarily composed of shale.

在这个地区，活跃的源岩主要由页岩组成。

3.The exploration team was excited to discover a new active source rock (活跃的源岩) formation.

勘探小组发现一个新的活跃的源岩层，感到非常兴奋。

4.The analysis revealed that the active source rock (活跃的源岩) has a high thermal maturity level.

分析显示，该活跃的源岩具有较高的热成熟度。

5.The geologists identified an area with abundant hydrocarbons, indicating the presence of active source rock (活跃的源岩).

地质学家们确认了一个富含碳氢化合物的区域，表明存在活跃的源岩。

作文

The study of geology often reveals fascinating insights into the processes that shape our planet. Among these processes, the formation of hydrocarbons—such as oil and natural gas—is particularly significant. One crucial component in this process is the concept of active source rock, which refers to sedimentary rock that has generated and expelled hydrocarbons. Understanding this term is vital for geologists and petroleum engineers alike, as it plays a pivotal role in the exploration and production of fossil fuels.To grasp the importance of active source rock, we must first understand how hydrocarbons are formed. Over millions of years, organic materials, primarily from ancient marine organisms, accumulate on the seabed. As layers of sediment build up over time, the pressure and temperature increase, leading to the transformation of these organic materials into hydrocarbons. The rocks that contain these organic materials are known as source rocks. However, not all source rocks are created equal; only those that continue to generate and release hydrocarbons are classified as active source rock.The characteristics of active source rock include high organic content, appropriate thermal maturity, and a suitable geological setting. The organic content must be sufficient to generate hydrocarbons, while thermal maturity refers to the degree to which the organic matter has been heated. If the temperature is too low, the hydrocarbons will not form, and if it is too high, the hydrocarbons may break down into simpler compounds. Therefore, the ideal conditions for an active source rock are a delicate balance of temperature and pressure.Geologists often utilize various techniques to identify and evaluate active source rock. One common method is the analysis of rock samples through techniques like gas chromatography and mass spectrometry. These methods allow scientists to determine the type and quantity of hydrocarbons present in the rock, as well as its maturity level. This information is crucial for assessing the potential of a geological formation for oil and gas production.Moreover, the location of active source rock is equally important. It is often found in basins where the right conditions for sediment accumulation and organic matter preservation exist. For instance, many of the world's most productive oil fields are located in areas where active source rock is abundant. This is why understanding the distribution of these rocks is essential for effective resource management and exploration strategies.In conclusion, the term active source rock encapsulates a critical aspect of hydrocarbon generation and extraction. By comprehending the processes that lead to the formation of these rocks, geologists can better predict where to find oil and gas deposits. As energy demands continue to rise globally, the significance of active source rock will only grow, making it an essential topic of study within the field of geology. The ongoing research and advancements in technology will undoubtedly enhance our understanding of these geological formations, leading to more efficient and sustainable methods of energy production in the future.

地质学的研究常常揭示出塑造我们星球过程的迷人见解。在这些过程中，烃类（如石油和天然气）的形成尤为重要。在这个过程中，一个关键的组成部分是“活跃源岩”的概念，它指的是已经生成并排放烃类的沉积岩。理解这个术语对于地质学家和石油工程师来说至关重要，因为它在化石燃料的勘探和生产中扮演着核心角色。要掌握“活跃源岩”的重要性，我们首先必须了解烃类是如何形成的。数百万年来，主要来自古代海洋生物的有机材料在海底积累。随着沉积层随时间的推移不断堆积，压力和温度增加，导致这些有机材料转化为烃类。含有这些有机材料的岩石被称为源岩。然而，并非所有源岩都是相同的；只有那些继续生成和释放烃类的岩石才被归类为“活跃源岩”。“活跃源岩”的特征包括高有机质含量、适当的热成熟度和合适的地质环境。有机质含量必须足够以生成烃类，而热成熟度则指有机物的加热程度。如果温度过低，烃类将不会形成；如果温度过高，烃类可能会分解成更简单的化合物。因此，“活跃源岩”的理想条件是温度和压力的微妙平衡。地质学家常常利用各种技术来识别和评估“活跃源岩”。一种常见的方法是通过气相色谱和质谱等技术分析岩石样本。这些方法使科学家能够确定岩石中存在的烃类类型和数量，以及其成熟度水平。这些信息对于评估某一地质构造的石油和天然气生产潜力至关重要。此外，“活跃源岩”的位置同样重要。它通常位于沉积物积累和有机物保存的合适条件存在的盆地中。例如，世界上许多最具生产力的油田都位于“活跃源岩”丰富的地区。这就是为什么理解这些岩石的分布对于有效的资源管理和勘探策略至关重要。总之，术语“活跃源岩”概括了烃类生成和提取的一个关键方面。通过理解导致这些岩石形成的过程，地质学家可以更好地预测在哪里找到石油和天然气储藏。随着全球能源需求的持续上升，“活跃源岩”的重要性只会增加，使其成为地质学领域内一个必不可少的研究主题。持续的研究和技术进步无疑将增强我们对这些地质构造的理解，从而在未来实现更高效和可持续的能源生产方法。