diapiric

简明释义

英[daɪˈæpərɪk]美[daɪˈæpərɪk]

adj. 挤入的

英英释义

单词用法

同义词

反义词

例句

1.Being its extra geological qualities, special oil gas reservoir come into being extensively over the mud diapiric structure belt.

其特有的地质特征使泥底辟构造带广泛形成具有特色的油气藏。

2.The Paleogene tectonic framework in Bohai Bay was controlled by both Mesozoic sinistral strike slip and Paleogene extension resulted from diapiric intrusion of mantle.

中生代左行走滑和早第三纪伸展作用共同控制了渤海海域早第三纪的构造格局。

3.And understanding the ore controlled by diapiric structure has started a new route for the ore prospecting work in the Kunyang Group.

认识刺穿构造控矿，为在昆阳群内的找矿工作开辟了新的途径。

4.The Paleogene tectonic framework in Bohai Bay was controlled by both Mesozoic sinistral strike slip and Paleogene extension resulted from diapiric intrusion of mantle.

中生代左行走滑和早第三纪伸展作用共同控制了渤海海域早第三纪的构造格局。

5.The basin consists of central diapiric zone and a slope zone.

该盆地由中央底辟带和斜坡带两个构造单元组成。

6.It is Iocated in a diapiric structure, controlled by structure, with a primary Cu deposition basis, and enriched by the later superimposed reformation.

它是位于刺穿构造内，以原始铜沉积为基础，受构造控制的后期叠加改造富化矿床。

7.The traps were formed by the upward arch of diapiric fluid, and episodic diapir activity determined hydrocarbon episodic migration.

主要圈闭由底辟流体上拱形成，底辟活动的幕式发育决定了油气幕式运移。

8.Geologists often study diapiric 岩脉的 structures to understand the behavior of salt domes.

地质学家经常研究diapiric 岩脉的结构，以了解盐丘的行为。

9.The diapiric 岩脉的 rise is often associated with the buoyancy of low-density materials.

diapiric 岩脉的上升通常与低密度材料的浮力有关。

10.The diapiric 岩脉的 activity can create unique geological formations in sedimentary basins.

在沉积盆地中，diapiric 岩脉的活动可以形成独特的地质构造。

11.During the field trip, we observed several diapiric 岩脉的 features that indicated past tectonic activity.

在实地考察中，我们观察到几个diapiric 岩脉的特征，这表明过去的构造活动。

12.The formation of the mountain range was influenced by a series of diapiric 岩脉的 movements beneath the Earth's crust.

这座山脉的形成受到了地壳下方一系列diapiric 岩脉的运动的影响。

作文

In the study of geology, the term diapiric refers to a specific geological process that involves the upward movement of a viscous material, such as salt or magma, through overlying layers of less dense rock. This phenomenon is significant in understanding various geological formations and the dynamics of Earth's crust. The process of diapiric movement can create unique structures and features that are essential for geologists to analyze when studying the history of an area.The concept of diapiric formations can be observed in various locations around the world. For example, salt domes, which are often found in sedimentary basins, are classic examples of diapiric structures. These salt domes form when salt deposits, being less dense than the surrounding sedimentary rocks, begin to rise through the overburden. As the salt moves upward, it can deform the surrounding strata, creating a variety of geological features such as folds and faults. Understanding these diapiric processes is crucial for resource exploration, particularly in the search for hydrocarbons and other minerals.The significance of diapiric movement extends beyond just the formation of salt domes. In volcanic regions, magma can also rise through the crust in a diapiric manner, leading to the formation of volcanoes. When magma ascends through the surrounding rock, it can cause fracturing and other changes in the geological structure, ultimately resulting in volcanic eruptions. This aspect of diapiric behavior highlights the dynamic nature of the Earth’s interior and the continuous processes that shape our planet.Moreover, the study of diapiric structures can provide valuable insights into past geological events. By examining the characteristics of diapiric formations, geologists can infer information about the pressures and temperatures that existed in the Earth’s crust at different times. This knowledge is vital for reconstructing the geological history of an area and understanding how it has evolved over millions of years.In addition to its geological implications, the concept of diapiric movement can also be applied metaphorically in other fields. For instance, in the realm of social sciences, one might describe certain social movements as diapiric if they involve a gradual rise of ideas or trends through layers of societal norms and expectations. This analogy emphasizes the idea that just as geological materials can force their way upward, so too can innovative ideas challenge and reshape established structures in society.In conclusion, the term diapiric encompasses a fascinating geological process that reveals much about the workings of our planet. From the formation of salt domes to volcanic activity, the implications of diapiric movement are profound and far-reaching. Furthermore, the metaphorical application of this concept in other disciplines serves to highlight the interconnectedness of various fields of study. Understanding diapiric processes not only enriches our knowledge of geology but also encourages us to think critically about the dynamics of change in any context.

在地质学的研究中，术语diapiric指的是一种特定的地质过程，涉及到粘性物质（如盐或岩浆）通过上方较轻的岩石层向上移动。这一现象对于理解各种地质构造和地球地壳的动态具有重要意义。diapiric运动的过程可以形成独特的结构和特征，这对地质学家在研究某个地区的历史时至关重要。diapiric构造的概念可以在世界各地的不同地点观察到。例如，盐丘通常在沉积盆地中发现，是diapiric结构的经典例子。这些盐丘形成于盐矿床因其密度低于周围沉积岩而开始上升。当盐向上移动时，它可以变形周围的岩层，形成各种地质特征，如褶皱和断层。理解这些diapiric过程对于资源勘探尤其重要，特别是在寻找碳氢化合物和其他矿物方面。diapiric运动的重要性不仅限于盐丘的形成。在火山区域，岩浆也可以以diapiric的方式通过地壳上升，导致火山的形成。当岩浆穿过周围的岩石上升时，会导致断裂和地质结构的其他变化，最终导致火山喷发。这一diapiric行为的这一方面突显了地球内部的动态特性及塑造我们星球的连续过程。此外，研究diapiric结构还可以提供关于过去地质事件的宝贵见解。通过检查diapiric构造的特征，地质学家可以推断出在不同时间地壳内存在的压力和温度信息。这些知识对于重建一个地区的地质历史和理解其数百万年来的发展至关重要。除了其地质意义外，diapiric运动的概念也可以在其他领域进行隐喻性应用。例如，在社会科学领域，如果某些社会运动涉及到思想或趋势通过社会规范和期望的层次逐渐上升，可以将其描述为diapiric。这种类比强调了这样一个观点：正如地质材料可以强行向上移动，创新思想也可以挑战并重塑社会中的既定结构。总之，术语diapiric涵盖了一种迷人的地质过程，揭示了我们星球运作的许多方面。从盐丘的形成到火山活动，diapiric运动的影响深远且广泛。此外，这一概念在其他学科中的隐喻性应用强调了各种研究领域之间的相互联系。理解diapiric过程不仅丰富了我们对地质学的知识，也鼓励我们批判性地思考任何背景下变革的动态。