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相关概念视频

Plotting of Topographic Maps01:29

Plotting of Topographic Maps

Topographic maps represent the Earth's surface features using contour lines, which connect points of equal elevation to create a two-dimensional representation of three-dimensional terrain. Creating a topographic map requires a systematic approach.Begin by plotting a scaled grid and marking intersections corresponding to the survey's elevation data points. Assign elevation values at these intersections to build the base map. Next, determine contour levels using a consistent contour interval,...
Coordinates and Map Projections01:29

Coordinates and Map Projections

Coordinates and map projections are essential tools in accurately representing the Earth's surface for various applications, ranging from navigation to spatial analysis. The latitude and longitude coordinate system is a universally recognized framework for defining locations. Latitude specifies the distance of a point north or south of the equator, measured in degrees from 0° at the equator to 90° at the poles. Longitude indicates a location's position east or west of the prime meridian,...
Gradient Fields01:27

Gradient Fields

A gradient field is a vector field derived from a scalar field. A scalar field assigns a single numerical value to every point in space, such as temperature, pressure, or electric potential. The gradient field describes how that value changes from point to point. It gives both the direction of the fastest increase and the rate of change in that direction.For a scalar field f(x, y), the gradient is written as\begin{equation*}\nabla f=\left\langle \jfrac{\partial f}{\partial x},\jfrac{\partial...
Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
Equipotential Surfaces and Field Lines01:29

Equipotential Surfaces and Field Lines

Electric potential can be pictorially represented as a three-dimensional surface. On such a surface, the electric potential is constant everywhere. The equipotential surface is always perpendicular to the electric field lines, and while it is three-dimensional, it can be treated as an equipotential line in a two-dimensional case. These equipotential lines are also always perpendicular to electric field lines. The term equipotential is often used as a noun, referring to an equipotential line or...
Three-Dimensional Analysis of Strain01:29

Three-Dimensional Analysis of Strain

Three-dimensional strain analysis is crucial for understanding how materials deform under stress, particularly in elastic, homogeneous materials. This method employs principal stress axes to simplify complex stress states into more understandable forms. Subjected to stress, a small cubic element within a material either expands or contracts along these axes, transforming into a rectangular parallelepiped. This transformation effectively illustrates the material's deformation. The principal...

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相关实验视频

Updated: Jul 11, 2026

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

板块构造学和热点:第三维空间

D L Anderson, T Tanimoto, Y S Zhang

    Science (New York, N.Y.)
    |June 19, 1992
    PubMed
    概括

    高分辨率的地震模型显示,上层地幔在很大程度上是热的,而不仅仅是热点周围. 这些发现挑战了以前关于板块构造学和地幔动态学的假设.

    科学领域:

    • 地质物理学 地质物理学
    • 地震学 地震学
    • 板块构造学是一种板块构造学.

    背景情况:

    • 上层地幔的热结构影响板块构造和岩石运动.
    • 之前的模型经常假设一个均的或同热的天气层.

    研究的目的:

    • 通过地震断层扫描,为板块构造学和热点理论提供新的约束.
    • 为了研究上层地幔的热结构和组成.

    主要方法:

    • 高分辨率的地震断层扫描被用于成像上层地幔.
    • 在不同深度对地震速度异常的分析.

    主要成果:

    • 中洋山脊表现出低地震速度 (深度<100公里),表明部分融化.
    • 更深层的异常与过去的山脊和沟迁移有关.
    • 扩展,裂和热点区域显示了深度低速度异常 (>200公里).
    • 上层地幔中的高速区域与古老的坑相对应.

    结论:

    • 上层地幔由巨大的热域组成,而不仅仅是小型热点区域.
    • 天气层是异质的,而不是异热的.

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    Atom Probe Tomography Analysis of Exsolved Mineral Phases

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    相关实验视频

    Last Updated: Jul 11, 2026

    Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
    07:58

    Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

    Published on: August 7, 2017

    Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
    06:55

    Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

    Published on: August 5, 2016

    Atom Probe Tomography Analysis of Exsolved Mineral Phases
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    Atom Probe Tomography Analysis of Exsolved Mineral Phases

    Published on: October 25, 2019

  • 岩石的形成取决于上层地幔的温度和石层条件.