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Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

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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...
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Region of Convergence of Laplace Tarnsform01:20

Region of Convergence of Laplace Tarnsform

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The Region of Convergence (ROC) is a fundamental concept in signal processing and system analysis, particularly associated with the Laplace transform. The ROC represents an area in the complex plane where the Laplace transform of a given signal converges, determining the transform's applicability and utility.
Consider a decaying exponential signal that begins at a specific time. When deriving its Laplace transform, the time-domain variable is replaced with a complex variable. This...
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Relative Motion Analysis - Acceleration01:10

Relative Motion Analysis - Acceleration

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A slider-crank mechanism converts rotational motion from the crank into linear motion of the slider or vice versa. This mechanism consists of three main parts: the crank, the connecting rod, and the slider. The movement of the slider-crank is an example of general plane motion as the fluctuating angle between the crank and the connecting rod. Consider a segment AB where point A is at the end of the slider and point B is on the diametrically opposite end to point A, on a crack. The variance in...
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Acceleration Vectors

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In everyday conversation, accelerating means speeding up. Acceleration is a vector in the same direction as the change in velocity, Δv, therefore the greater the acceleration, the greater the change in velocity over a given time. Since velocity is a vector, it can change in magnitude, direction, or both. Thus acceleration is a change in speed or direction, or both. For example, if a runner traveling at 10 km/h due east slows to a stop, reverses direction, and continues their run at 10 km/h...
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Acceleration due to Gravity on Earth01:21

Acceleration due to Gravity on Earth

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According to Newton's law of gravitation, the gravitational force on a body is proportional to its mass. According to Newton's second law of motion, the acceleration produced by an external force is inversely proportional to the force. Hence, the acceleration of an object under an external force of gravitation is independent of its mass.
The acceleration of an object close to the Earth, because of the Earth's gravitational pull, is called the acceleration due to gravity. It is...
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Variation in Acceleration due to Gravity near the Earth's Surface01:20

Variation in Acceleration due to Gravity near the Earth's Surface

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An object's apparent weight is its weight measured by a spring balance at its location. It is different from its true weight, the force with which the Earth pulls it, because of the Earth's rotation. Mathematically, an object's apparent weight equals its true weight minus the centripetal force that keeps it in a circular motion along with the Earth's surface every 24 hours.
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関連する実験動画

Updated: Jun 8, 2025

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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パッシブ・マージン沈殿によるインド・ユーラシア収束の加速

Hao Zhou1, Jiashun Hu2,3, Luca Dal Zilio4,5

  • 1Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen, China.

Nature
|November 7, 2024
PubMed
まとめ

インド・ユーラシアの急速な収束は,約6500万年前に加速した. この地質学的な出来事は 最初の衝突を 約6000万年前に制限しました

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Last Updated: Jun 8, 2025

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科学分野:

  • 地質学
  • 地理学
  • 地化学

背景:

  • 約6500万年前,インドプレートとユーラシアプレートの間の加速的な収束は,複雑な地質学的な出来事です.
  • 前回の説明では プレート速度に影響を与える 構造の歴史や力について 不確実性がありました

研究 の 目的:

  • インド-ユーラシアの収束率の急速な増加を説明するために 65 Ma.
  • この加速における沈殿物の役割を調査する.

主な方法:

  • ガンジス岩の地化学分析 (同位体と微量元素)
  • 沈殿物の沈殿効果をシミュレートするための地動力学モデル.
  • マントル源への沈殿物溶融の寄与の分析

主要な成果:

  • ガンジス岩のマントル源に土着の沈殿物の融解による貢献は,約65万年前に観察された.
  • 数学的実験では,厚い堆積物 (1 km以上) の沈殿が,収束と地殻の拡張を促す可能性があることが示された.
  • 収束の加速は,受動的縁から派生した沈殿物の到着と相関しています.

結論:

  • インドとユーラシアの収束の急速な加速は,インド北部の被動地殻からの沈殿によって説明されます.
  • インドとユーラシアの衝突は,約60万年前に限られている.
  • コンチネンタル・アセンブリの最終段階では,一時的な潜水速度加速が一般的です.