ancillary depocenter

简明释义

1. 辅助沉积中心; 2. 次要沉积中心;

英英释义

例句

1.The team focused their drilling efforts on the ancillary depocenter 辅助沉积中心 to maximize their chances of finding hydrocarbons.

团队将钻探工作集中在 辅助沉积中心 ancillary depocenter 上，以最大化发现烃类的机会。

2.In the context of basin analysis, identifying the ancillary depocenter 辅助沉积中心 can help predict future resource locations.

在盆地分析的背景下，识别 辅助沉积中心 ancillary depocenter 可以帮助预测未来资源的位置。

3.The geological survey indicated that the ancillary depocenter 辅助沉积中心 was crucial for understanding sediment distribution.

地质调查显示，辅助沉积中心 ancillary depocenter 对理解沉积分布至关重要。

4.Mapping the ancillary depocenter 辅助沉积中心 allowed scientists to better understand sedimentary processes.

绘制 辅助沉积中心 ancillary depocenter 的图谱使科学家能够更好地理解沉积过程。

5.Researchers found that the ancillary depocenter 辅助沉积中心 played a significant role in the formation of local oil reservoirs.

研究人员发现，辅助沉积中心 ancillary depocenter 在当地油气藏的形成中起到了重要作用。

作文

The concept of an ancillary depocenter is crucial in the field of geology, particularly in sedimentology and stratigraphy. An ancillary depocenter refers to a secondary area where sediments are deposited, often influenced by the primary depocenter. Understanding this concept helps geologists interpret the sedimentary processes and the geological history of a region. In many cases, the main depocenter represents the primary location where sediments accumulate due to various factors such as water flow, tectonic activity, or climatic conditions. However, the existence of ancillary depocenters can provide insights into the dynamics of sediment transport and deposition that occur in conjunction with the primary processes.For instance, in river systems, the main channel may serve as the primary depocenter where most of the sediment is deposited. Yet, adjacent floodplains or backswamps can function as ancillary depocenters, capturing sediment during periods of high flow or flooding. This duality of sediment deposition highlights the complexity of sedimentary environments and the need for detailed analysis when studying geological formations.Moreover, recognizing ancillary depocenters can aid in resource exploration, such as hydrocarbons or minerals. In some basins, the primary depocenter may be well-known, but it is often the ancillary depocenters that hold untapped resources. By mapping these areas, geologists can identify new prospects for drilling or mining, which can have significant economic implications.In addition to practical applications, the study of ancillary depocenters contributes to our understanding of past environmental conditions. By analyzing sediment cores from these areas, scientists can reconstruct historical climate patterns, sea-level changes, and even ecological shifts. This information is invaluable for predicting future trends and preparing for potential environmental challenges.In conclusion, the term ancillary depocenter encompasses a vital aspect of sedimentary geology. It emphasizes the importance of secondary sediment deposition zones that complement primary locations. By studying both types of depocenters, researchers can gain a more comprehensive understanding of sediment dynamics, enhance resource exploration efforts, and reconstruct past environmental conditions. The significance of ancillary depocenters cannot be understated, as they play a critical role in shaping the geological landscape and informing us about Earth's history.

“副沉积中心”这一概念在地质学领域，尤其是在沉积学和地层学中至关重要。“副沉积中心”指的是一个次要的沉积区域，通常受到主要沉积中心的影响。理解这一概念有助于地质学家解读沉积过程及某一地区的地质历史。在许多情况下，主要沉积中心代表了由于水流、构造活动或气候条件等各种因素而沉积物积累的主要位置。然而，“副沉积中心”的存在可以提供有关与主要过程同时发生的沉积运输和沉积动态的见解。例如，在河流系统中，主河道可能作为主要沉积中心，在这里大部分沉积物被沉积。然而，邻近的洪泛平原或后沼泽可以作为“副沉积中心”，在高流量或洪水期间捕获沉积物。这种沉积的双重性突显了沉积环境的复杂性，并强调在研究地质形成时需要进行详细分析。此外，识别“副沉积中心”可以帮助资源勘探，例如碳氢化合物或矿物。在某些盆地中，主要沉积中心可能是众所周知的，但往往是“副沉积中心”蕴藏着尚未开发的资源。通过绘制这些区域的地图，地质学家可以识别新的钻探或采矿前景，这可能具有重大的经济意义。除了实际应用外，对“副沉积中心”的研究还促进了我们对过去环境条件的理解。通过分析这些地区的沉积物核心，科学家可以重建历史气候模式、海平面变化甚至生态转变。这些信息对于预测未来趋势和为潜在环境挑战做好准备是无价的。总之，“副沉积中心”一词涵盖了沉积地质学的一个重要方面。它强调了补充主要位置的次要沉积区域的重要性。通过研究这两种类型的沉积中心，研究人员可以更全面地了解沉积动态，增强资源勘探工作，并重建过去的环境条件。“副沉积中心”的重要性不容小觑，因为它们在塑造地质景观和告知我们地球历史方面发挥着关键作用。