isopach

简明释义

英[ˈaɪsəʊˌpæk]美[ˈaɪsəpæk]

n. [地质] 等厚线

英英释义

单词用法

同义词

反义词

例句

1.Authors draw and analyze depositional trend and strike sections and sandstone isopach maps by collecting a lot of bores.

通过收集大量钻孔资料，编制并分析了倾向沉积断面图、走向沉积断面图以及砂体等厚图。

2.After analysis of the isopach maps of restraining barrier thickness in each layers, four spread models of the restraining barriers in shallow water delta facies of the study area were built.

通过分析各层段的隔层厚度等值线图，建立了研究区浅水三角洲相隔层的四种展布模式。

3.In compiling areal isopach of a basin from seismic horizon structure map, we can use the residual thickness at both sides of fault plane to show the horizontal distribution of a fault.

在利用地震层位构造图编制盆地区域性等厚图时，可以用断层面的残留厚度来描绘断层在平面上的分布。

4.The terms isopach and isopach map are incorrectly used interchangeably to describe isochores and isochore maps.

但术语等厚线和等厚线图互换使用地来描述等层厚线和等层厚线图是不正确的。

5.Finally, the isopach map of the turbidite lens can be plotted by quantitatively interpreting the amplitudes on seismic sections using quantitative interpretation template made from seismic modeling.

利用地震模型制作的定量解释图板，对地震剖面上的振幅进行定量解释，最后可编制出砂岩透镜体等厚图。

6.Finally, the isopach map of the turbidite lens can be plotted by quantitatively interpreting the amplitudes on seismic sections using quantitative interpretation template made from seismic modeling.

利用地震模型制作的定量解释图板，对地震剖面上的振幅进行定量解释，最后可编制出砂岩透镜体等厚图。

7.Using the isopach data, we can identify potential areas for oil exploration.

通过使用等厚线数据，我们可以确定潜在的石油勘探区域。

8.Engineers used the isopach model to assess the stability of the foundation for the new building.

工程师们使用等厚线模型来评估新建筑基础的稳定性。

9.The geologist created an isopach map to show the thickness of sedimentary layers in the region.

地质学家制作了一张等厚线地图，以显示该地区沉积层的厚度。

10.The isopach analysis revealed significant variations in rock thickness across the basin.

该等厚线分析揭示了盆地内岩石厚度的显著变化。

11.The isopach map was instrumental in understanding the geological history of the area.

这张等厚线地图对于理解该地区的地质历史至关重要。

作文

In the field of geology and geophysics, understanding various geological features is crucial for resource exploration and environmental studies. One important term that often arises in this context is isopach, which refers to a line on a map connecting points of equal thickness of a particular stratum or layer of rock. This concept is vital for geologists as it helps them visualize the distribution of sedimentary layers and their thickness across a given area. The study of isopach maps can reveal much about the geological history of a region, including past environments and tectonic activities.When creating an isopach map, geologists typically gather data from various boreholes and seismic surveys. Each borehole provides information on the depth and thickness of different layers of rock, which can then be plotted on a map. By connecting these points, geologists can create a visual representation of how thick each layer is across a larger area. This is particularly useful in the oil and gas industry, where understanding the thickness of reservoir rocks can determine whether a site is worth drilling.Moreover, isopach maps are not only used in hydrocarbon exploration but also in assessing groundwater resources. By analyzing the thickness of aquifer layers, hydrologists can make informed decisions regarding water extraction and management. In regions where water scarcity is a concern, knowing the thickness of aquifers can help in planning sustainable water use.The interpretation of isopach maps also plays a role in understanding sedimentary processes. For example, a thick layer of sediment in a specific area may indicate a historical river delta or a marine environment where sediments were deposited over time. Conversely, thin layers could suggest erosion or a lack of sediment supply. Thus, isopach maps serve as a valuable tool for reconstructing past geological events and environments.In addition to their practical applications, isopach maps also contribute to academic research. Geologists often publish studies that include isopach maps to support their findings regarding regional geology, stratigraphy, and paleoenvironments. These publications can enhance our understanding of Earth's history and the processes that have shaped its surface.In conclusion, the term isopach encapsulates a fundamental aspect of geological mapping that aids in the exploration and understanding of subsurface resources. By connecting points of equal thickness, geologists can visualize and interpret the distribution of different strata, which is essential for various applications, from resource extraction to environmental management. As we continue to study and explore our planet, the significance of isopach maps will undoubtedly remain a cornerstone of geological science and research.

在地质学和地球物理学领域，理解各种地质特征对于资源勘探和环境研究至关重要。一个常常出现的重要术语是等厚线，它指的是在地图上连接特定岩层或岩石层相等厚度的点的线。这个概念对地质学家来说是至关重要的，因为它帮助他们可视化沉积层的分布及其在给定区域内的厚度。对等厚线图的研究可以揭示一个地区的地质历史，包括过去的环境和构造活动。在制作等厚线图时，地质学家通常会从各种钻孔和地震勘测中收集数据。每个钻孔提供有关不同岩层深度和厚度的信息，这些信息可以绘制在地图上。通过连接这些点，地质学家可以创建一个视觉表示，显示每层在更大区域内的厚度。这在石油和天然气行业中特别有用，因为了解储层岩石的厚度可以决定一个地点是否值得钻探。此外，等厚线图不仅用于碳氢化合物勘探，还用于评估地下水资源。通过分析含水层的厚度，水文学家可以就水的提取和管理做出明智的决策。在水资源短缺的问题严重的地区，了解含水层的厚度可以帮助规划可持续的水使用。对等厚线图的解释也在理解沉积过程方面发挥着作用。例如，某一特定区域的厚沉积层可能表明历史上的河口三角洲或沉积物沉积的海洋环境。相反，薄层可能表明侵蚀或沉积物供应不足。因此，等厚线图作为重建过去地质事件和环境的有价值工具。除了实际应用外，等厚线图还为学术研究做出了贡献。地质学家经常发表包含等厚线图的研究，以支持他们关于区域地质、地层学和古环境的发现。这些出版物可以增强我们对地球历史及其表面塑造过程的理解。总之，术语等厚线概括了地质制图的一个基本方面，帮助探索和理解地下资源。通过连接相等厚度的点，地质学家可以可视化和解释不同岩层的分布，这对各种应用至关重要，从资源开采到环境管理。随着我们继续研究和探索我们的星球，等厚线图的重要性无疑将继续成为地质科学和研究的基石。