anticlinoria
简明释义
英[ˌæntɪklaɪˈnɔriə]美[ˌæntɪklaɪˈnɔriə]
n. 复背斜;复背斜层(anticlinorium 的变形)
英英释义
单词用法
同义词
背斜 | 背斜结构常常在地质学中研究。 | ||
褶皱 | 地壳中的褶皱可以指示构造活动。 |
反义词
例句
1.The Haiyangshan granitic mass was intruded in the core of anticlinoria and formed in the late Silurian.
广西海洋山花岗岩基侵位于海洋山复式背斜核部,形成于晚志留世。
2.The Haiyangshan granitic mass was intruded in the core of anticlinoria and formed in the late Silurian.
广西海洋山花岗岩基侵位于海洋山复式背斜核部,形成于晚志留世。
3.The formation of anticlinoria can be attributed to tectonic forces acting over millions of years.
背斜的形成可以归因于数百万年来作用于地壳的构造力量。
4.The geological survey revealed an extensive area of anticlinoria which indicates the presence of folded rock layers.
地质调查显示出一大片背斜区域,表明存在折叠的岩层。
5.In studying the region, we found that the anticlinoria played a crucial role in the local ecosystem.
在研究该地区时,我们发现背斜在当地生态系统中起着至关重要的作用。
6.The research team focused on the anticlinoria to understand the sedimentary processes involved.
研究小组专注于背斜以理解相关的沉积过程。
7.Geologists often use satellite imagery to identify anticlinoria in remote areas.
地质学家常常使用卫星图像来识别偏远地区的背斜。
作文
Understanding geological structures is crucial for various fields such as geology, engineering, and environmental science. One such structure that often intrigues geologists is the anticlinoria, which refers to a large-scale geological feature characterized by a series of anticlines that can extend over vast areas. An anticline itself is a type of fold that is arch-like in shape, where the oldest rock layers are found at the core, and younger layers are found on the flanks. The study of anticlinoria provides insights into the tectonic forces that shape our planet and can reveal important information about the history of the Earth’s crust.The significance of anticlinoria lies not only in their geological implications but also in their economic value. Many natural resources, including oil, gas, and minerals, are often found in association with these structures. For instance, the oil industry frequently targets anticlinoria because the folded rock layers can trap hydrocarbons, making them potential reservoirs. Understanding the formation and distribution of anticlinoria is therefore essential for resource exploration and management.From a geological perspective, anticlinoria typically form as a result of compressional forces that cause the Earth's crust to buckle. This process can occur over millions of years, leading to the development of complex structures that can vary significantly in size and shape. The identification and mapping of anticlinoria are critical tasks for geologists, as they help in understanding the regional geology and the processes that have shaped a particular area.Moreover, the study of anticlinoria can also provide valuable information regarding seismic activity. Areas with significant folding and faulting, including anticlinoria, are often more susceptible to earthquakes. By studying these geological features, scientists can better assess the risks associated with seismic events and develop strategies for mitigation. This knowledge is particularly important in regions where populations are dense and infrastructure is vulnerable to natural disasters.In addition to their geological and economic importance, anticlinoria can also contribute to the aesthetic value of landscapes. Many scenic vistas are formed by the dramatic folds and valleys associated with these structures. For instance, national parks and protected areas often showcase stunning examples of anticlinoria, attracting tourists and nature enthusiasts alike. The interplay of light and shadow across the folds can create breathtaking views that highlight the beauty of geological processes.In conclusion, the term anticlinoria encapsulates a fascinating aspect of geology that intertwines the Earth's history, resource management, and even aesthetics. As we continue to explore and understand these geological features, we gain a deeper appreciation for the dynamic processes that shape our planet. Whether it is through resource exploration, risk assessment, or simply enjoying the beauty of the landscape, the study of anticlinoria remains a vital part of geological science and its applications in the modern world.
有效理解和掌握地质结构对于地质学、工程学和环境科学等多个领域至关重要。其中一个常常引起地质学家兴趣的结构是anticlinoria,它指的是一种以一系列背斜为特征的大规模地质特征,这些背斜可以延伸到广阔的区域。背斜本身是一种折叠结构,呈拱形,其中心是最古老的岩层,而年轻的岩层则位于侧翼。对anticlinoria的研究提供了对塑造我们星球的构造力的洞察,并能揭示关于地壳历史的重要信息。anticlinoria的重要性不仅体现在其地质意义上,还体现在其经济价值上。许多自然资源,包括石油、天然气和矿产,通常与这些结构相关联。例如,石油行业经常瞄准anticlinoria,因为折叠的岩层可以捕获碳氢化合物,使其成为潜在的储层。因此,理解anticlinoria的形成和分布对于资源勘探和管理至关重要。从地质角度来看,anticlinoria通常是由于压缩力导致地壳弯曲而形成的。这个过程可能持续数百万年,导致形成复杂的结构,大小和形状可能有显著差异。识别和绘制anticlinoria是地质学家的关键任务,因为它们有助于理解区域地质及塑造特定区域的过程。此外,anticlinoria的研究还可以提供有关地震活动的宝贵信息。具有显著折叠和断裂的地区,包括anticlinoria,通常更易发生地震。通过研究这些地质特征,科学家可以更好地评估与地震事件相关的风险,并制定减灾策略。这一知识在密集人口和基础设施易受自然灾害影响的地区尤其重要。除了地质和经济重要性外,anticlinoria也可以增强景观的美学价值。许多风景如画的景观是由这些结构相关的戏剧性折叠和山谷形成的。例如,国家公园和保护区通常展示令人惊叹的anticlinoria实例,吸引游客和自然爱好者。光与影在折叠之间的交错可以创造出令人叹为观止的视野,突显地质过程的美。总之,术语anticlinoria概括了地质学中一个迷人的方面,它交织了地球的历史、资源管理,甚至美学。随着我们继续探索和理解这些地质特征,我们对塑造我们星球的动态过程有了更深刻的认识。无论是通过资源勘探、风险评估,还是单纯享受风景的美丽,anticlinoria的研究仍然是地质科学及其在现代世界应用的重要组成部分。