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関連する概念動画

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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関連する実験動画

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

プレート構造とホットスポット:第3次元

D L Anderson, T Tanimoto, Y S Zhang

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

    高解像度の地震モデルは,ホットスポットの周りに限らず,上層マントルが主に熱いことを明らかにしています. これらの発見は,プレート構造学とマントルの動力学に関する以前の仮定に異議を唱える.

    科学分野:

    • 地質物理学 地質物理学とは地質物理学です.
    • 地震学 地震学とは
    • プレート・テクトニクス (プレート・テクトニクス)

    背景:

    • 上層マントルの熱構造はプレート構造とマグマティズムに影響を与えます.
    • 以前のモデルは,しばしば均質または同熱のアステノスフィアを想定していた.

    研究 の 目的:

    • 地震トモグラフィーを用いてプレートテクトニクスとホットスポット理論に新たな制約を与える.
    • 上層マントルの熱的構造と構成を調査する.

    主な方法:

    • 高解像度地震トモグラフィーは上層マントルの画像を撮影するために使用されました.
    • 様々な深さでの地震速度の異常を分析する.

    主要な成果:

    • 中洋のは低地震速度 (深さ<100 km) を表しており,部分的に溶けていることを示している.
    • より深い異常は,過去の山脊と溝の移動と相関しています.
    • エクステンション,リフト,ホットスポット領域は,低速度の異常 (>200 km) を示す.
    • 上層マントルの高速度領域は,アーキア紀のクラトンと相関しています.

    結論:

    さらに関連する動画

    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
    08:14

    Atom Probe Tomography Analysis of Exsolved Mineral Phases

    Published on: October 25, 2019

    関連する実験動画

    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
    08:14

    Atom Probe Tomography Analysis of Exsolved Mineral Phases

    Published on: October 25, 2019

    • 上層マントルは,小さなホットスポット地域だけでなく,広大なホットドメインで構成されています.
    • アステノスフィアは異質であり,同熱ではない.
    • マグマティズムは上層マントルの温度と石層の条件の両方に依存しています.