synclinal

简明释义

英[sɪŋˈklaɪn(ə)l]美[sɪnˈklaɪnəl]

adj. 向斜的，倾斜的

英英释义

单词用法

同义词

反义词

例句

1.The Sankeng geothermal field is located on the northeastern side of the Wuchuan Sihui deep fault and in the Sankeng synclinal karstic basin.

广东三坑地热田位于吴川—四会深大断裂带的东北侧，三坑向斜岩溶盆地内。

2.The experience of water danger reclamation in synclinal axis illustrating at T312 working face is introduced.

介绍了T312工作面向斜轴部水患治理的经验。

3.The Sankeng geothermal field is located on the northeastern side of the Wuchuan Sihui deep fault and in the Sankeng synclinal karstic basin.

广东三坑地热田位于吴川—四会深大断裂带的东北侧，三坑向斜岩溶盆地内。

4.The western tongue has a synclinal bottom configuration, the axis of which plunges at a low angle towards the fault.

（结晶学）有三个以倾斜的角度交叉的不同晶轴。

5.The team used satellite imagery to map out the synclinal 向下弯曲的地层 formations across the mountain range.

团队利用卫星图像绘制了整个山脉的synclinal 向下弯曲的地层形态图。

6.The geological survey revealed a large synclinal 向下弯曲的地层 structure in the region, indicating potential for natural resources.

地质调查显示该地区有一个大型的synclinal 向下弯曲的地层结构，表明可能存在自然资源。

7.The synclinal 向下弯曲的地层 features were critical in locating groundwater reservoirs.

这些synclinal 向下弯曲的地层特征对寻找地下水储存区至关重要。

8.When studying the rock formations, we identified several synclinal 向下弯曲的地层 patterns that helped us understand the area's geological history.

在研究岩石形态时，我们识别出几个synclinal 向下弯曲的地层模式，这帮助我们理解该地区的地质历史。

9.In structural geology, recognizing a synclinal 向下弯曲的地层 can indicate the presence of oil deposits.

在构造地质学中，识别出一个synclinal 向下弯曲的地层可以指示油藏的存在。

作文

In the study of geology, understanding the various formations and structures of the Earth's crust is crucial. One such formation is the synclinal, which refers to a type of fold in the rock layers where the younger rocks are found at the center of the fold, and the older rocks are located on the outer edges. This structure is essential for geologists as it provides insights into the geological history of an area. The synclinal formation typically occurs in regions that have experienced significant tectonic activity, resulting in the bending and folding of the Earth's crust. When we examine a synclinal fold, we can visualize it as a trough-like structure, where the layers of rock dip inward towards the center. This is in contrast to an anticlinal fold, where the layers arch upwards. Understanding these differences is vital for anyone studying geology, as they reveal much about the processes that have shaped our planet over millions of years. For instance, when conducting field studies, geologists often look for synclinal formations to identify potential sites for oil and gas deposits. The way these layers are arranged can trap hydrocarbons, making them key areas for exploration. Furthermore, the presence of a synclinal can indicate past environmental conditions, helping scientists reconstruct ancient landscapes and climates. In addition to their economic importance, synclinal formations also play a role in understanding natural hazards. Areas with pronounced folds may be more susceptible to landslides or earthquakes due to the stress placed on the rock layers. By studying these formations, researchers can better assess risks and develop strategies for mitigation. Moreover, the aesthetic beauty of synclinal landscapes cannot be overlooked. Many national parks feature stunning views of these geological structures, attracting tourists and nature enthusiasts alike. The interplay of light and shadow across the folds creates a dynamic visual experience, illustrating the power of natural forces over time. In conclusion, the concept of synclinal is integral to the field of geology. Its implications stretch beyond academic interest, influencing economic pursuits, environmental assessments, and even tourism. As we continue to explore and understand our planet, recognizing the significance of synclinal formations will remain a vital aspect of geological studies. By appreciating these structures, we not only gain knowledge about the Earth’s history but also foster a deeper connection to the natural world around us.

在地质学研究中，理解地壳的各种构造和形态至关重要。其中一种构造是synclinal，指的是岩石层中的一种褶皱结构，年轻的岩石位于褶皱的中心，而老的岩石则位于外缘。这种结构对地质学家来说非常重要，因为它提供了一个地区地质历史的见解。synclinal 形成通常发生在经历过显著构造活动的地区，导致地壳的弯曲和折叠。当我们检查synclinal 褶皱时，可以将其视为一种槽状结构，岩层向内倾斜，朝向中心。这与拱状褶皱（anticlinal）形成相反，后者的岩层向上拱起。理解这些差异对于任何学习地质学的人来说都是至关重要的，因为它们揭示了塑造我们星球数百万年来的过程。例如，在进行野外研究时，地质学家常常寻找synclinal 形成，以识别潜在的油气储藏地点。这些岩层的排列方式可以捕获碳氢化合物，使其成为勘探的关键区域。此外，synclinal 的存在可以指示过去的环境条件，帮助科学家重建古代景观和气候。除了经济重要性外，synclinal 形成在理解自然灾害方面也发挥着作用。具有明显褶皱的地区可能由于岩层上的压力而更容易发生滑坡或地震。通过研究这些形成，研究人员可以更好地评估风险并制定缓解策略。此外，synclinal 景观的美丽也不容忽视。许多国家公园以这些地质结构的壮丽景观而闻名，吸引了游客和自然爱好者。光与影在褶皱之间的交错创造出动态的视觉体验，展示了自然力量随着时间的推移所产生的影响。总之，synclinal 的概念对地质学领域至关重要。其影响超越了学术兴趣，影响着经济追求、环境评估甚至旅游业。随着我们继续探索和理解我们的星球，认识到synclinal 形成的重要性将始终是地质研究的一个重要方面。通过欣赏这些结构，我们不仅获得了关于地球历史的知识，还加深了与周围自然世界的联系。