synclinorium

简明释义

英[ˌsɪŋklɪˈnɔːrɪəm]美[ˌsɪŋklaɪˈnɔrɪəm]

n. [地质] 复向斜

复 数 s y n c l i n o r i a

英英释义

单词用法

同义词

反义词

例句

1.Nanshu graphite deposits, located at the south side of Qixia synclinorium in Jiaodong uplift, exist in Liujiazhuang marble member of Jingqishan formation, Jiaodong group of Archaeozic Erathern.

山东省莱西县南墅石墨矿位于胶东隆起栖霞复背斜的南翼，石墨赋存于太古界胶东群旌旗山组刘家庄大理岩段。

2.Nanshu graphite deposits, located at the south side of Qixia synclinorium in Jiaodong uplift, exist in Liujiazhuang marble member of Jingqishan formation, Jiaodong group of Archaeozic Erathern.

山东省莱西县南墅石墨矿位于胶东隆起栖霞复背斜的南翼，石墨赋存于太古界胶东群旌旗山组刘家庄大理岩段。

3.Based on above, the author point out that the central block of Chenghu-tuditang synclinorium and the southern block of Dangyang synclinorium are the advantageous regions for exploration.

在综合研究江汉平原石炭系—下三叠统油气成藏条件的基础上，指出了沉湖—土地堂复向斜中部区块、当阳复向斜南部区块为有利的勘探地区。

4.The geological survey revealed a large synclinorium in the region, indicating significant folding of the Earth's crust.

地质调查显示该地区有一个大型向斜构造，表明地壳发生了显著的褶皱。

5.Understanding the formation of a synclinorium can help geologists predict the location of natural resources.

理解向斜构造的形成可以帮助地质学家预测自然资源的位置。

6.The synclinorium was formed during the mountain-building processes millions of years ago.

这个向斜构造是在数百万年前的造山过程中形成的。

7.In sedimentary basins, a synclinorium often indicates areas of potential oil reserves.

在沉积盆地中，向斜构造通常表明潜在的石油储备区域。

8.The research team focused on mapping the synclinorium to understand its impact on local geology.

研究小组专注于绘制向斜构造的地图，以了解其对当地地质的影响。

作文

In the study of geology, understanding the various structures that form within the Earth's crust is crucial for comprehending how our planet has evolved over millions of years. One such structure is the synclinorium, which can be described as a large, complex geological formation characterized by a series of synclines that are arranged in a concave upward manner. This term derives from the combination of 'syncline'—a fold in rock layers that slopes downward from the crest—and 'orium', a suffix used to denote a place or region. Thus, a synclinorium represents a significant area where these downward-sloping folds are prevalent. The formation of a synclinorium often occurs due to tectonic forces acting on the Earth's crust, which can lead to the bending and folding of rock layers over time. As these forces work to shape the landscape, they create various geological features that can provide valuable insights into the history of the Earth’s surface. For instance, by studying the arrangement and composition of rocks within a synclinorium, geologists can infer the types of stress that were applied during its formation and the geological processes that have taken place since. One of the most interesting aspects of a synclinorium is its potential to host important natural resources. The specific arrangement of rock layers can create traps for oil and gas deposits, making these formations valuable for exploration and extraction. Additionally, the minerals found within the rocks can also be economically significant. Understanding the geological context of a synclinorium not only aids in resource management but also contributes to broader environmental studies, as these structures can influence local ecosystems and hydrology. Furthermore, the study of synclinoriums can enhance our understanding of seismic activity. Regions where these formations are present may exhibit unique patterns of earthquakes and tectonic movements. By analyzing the structural integrity of a synclinorium, scientists can better predict seismic hazards and develop strategies for risk mitigation in nearby communities. This is particularly relevant in areas where urban development is expanding into geologically active regions. In conclusion, the synclinorium is not just a term used by geologists; it embodies a wealth of information about the Earth's geological history and current processes. Its intricate structure tells a story of the dynamic forces that shape our planet, while also serving as a reminder of the natural resources and hazards that accompany such formations. As we continue to explore and study these geological phenomena, the importance of understanding terms like synclinorium becomes increasingly apparent, paving the way for advancements in geology, resource management, and environmental science.

在地质学的研究中，理解地壳内形成的各种结构对于理解我们星球在数百万年中的演变至关重要。其中一个这样的结构是synclinorium，可以描述为一种大型复杂的地质构造，其特征是由一系列向下凹陷的褶皱（即向下倾斜的褶皱）组成。这一术语源于“syncline”（即一种从山脊向下倾斜的岩层褶皱）和“orium”（一个用于表示地方或区域的后缀）的结合。因此，synclinorium代表了这些向下倾斜的褶皱普遍存在的重要区域。 synclinorium的形成通常是由于地壳上的构造力量作用，导致岩层随着时间的推移而弯曲和折叠。当这些力量作用于地貌时，它们会创造出各种地质特征，这些特征能够提供关于地球表面历史的宝贵见解。例如，通过研究synclinorium内部岩石的排列和成分，地质学家可以推断出在其形成过程中施加的应力类型以及自那时以来发生的地质过程。 synclinorium的一个有趣方面是它可能蕴藏着重要的自然资源。岩层的特定排列可以为石油和天然气储藏创造陷阱，使这些构造在勘探和开采中具有价值。此外，岩石中发现的矿物也可能具有经济重要性。理解synclinorium的地质背景不仅有助于资源管理，还有助于更广泛的环境研究，因为这些结构可能影响当地生态系统和水文情况。 此外，synclinorium的研究可以增强我们对地震活动的理解。这些构造存在的区域可能表现出独特的地震和构造运动模式。通过分析synclinorium的结构完整性，科学家可以更好地预测地震危险，并制定风险缓解策略，以保护附近社区。这在城市发展扩展到地质活跃地区时尤为相关。 总之，synclinorium不仅仅是地质学家使用的一个术语；它蕴含着关于地球地质历史和当前过程的丰富信息。其复杂的结构讲述了塑造我们星球的动态力量的故事，同时也提醒我们伴随这些构造而来的自然资源和危害。随着我们继续探索和研究这些地质现象，理解像synclinorium这样的术语的重要性变得愈发明显，为地质学、资源管理和环境科学的进步铺平了道路。