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関連する概念動画

Tidal Forces01:06

Tidal Forces

2.9K
The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to...
2.9K
Travelling Waves01:04

Travelling Waves

5.9K
A wave is a disturbance that propagates from its source, repeating itself periodically, and is typically associated with simple harmonic motion. Mechanical waves are governed by Newton's laws and require a medium to travel. A medium is a substance in which a mechanical wave propagates, and the medium produces an elastic restoring force when it is deformed.
Water waves, sound waves, and seismic waves are some examples of mechanical waves. For water waves, the wave propagation medium is...
5.9K
Shock Waves01:16

Shock Waves

2.1K
While deriving the Doppler formula for the observed frequency of a sound wave, it is assumed that the speed of sound in the medium is greater than the source's speed through it. When this condition is breached, a shock wave occurs.
When the source's speed approaches the speed of sound, constructive interference between successive wavefronts emitted by the source occurs immediately behind it. Initially, scientists believed that this constructive interference would result in such high...
2.1K
Rolling With Slipping01:14

Rolling With Slipping

6.9K
Rolling with slipping is a physical phenomenon that occurs when a rolling object experiences both rotational and linear motion but also experiences frictional forces that cause slipping. This phenomenon can occur in various situations, such as when a tire rolls on a wet road or a ball rolls on a rough surface.
An object's rolling motion is characterized by its rotation around its axis, while linear motion refers to the object's translational motion along a surface. Frictional forces can...
6.9K
Elastic Strain Energy for Shearing Stresses01:20

Elastic Strain Energy for Shearing Stresses

668
As discussed in previous lessons, strain energy in a material is the energy stored when it is elastically deformed, a concept crucial in materials science and mechanical engineering. This energy results from the internal work done against the cohesive forces within the material. When a material undergoes shearing stress and corresponding shearing strain, the strain energy density, which is the energy stored per unit volume, is calculated. Within the elastic limit, where the stress is...
668
Fault Types01:18

Fault Types

601
When analyzing a single line-to-ground fault from phase A to ground at a three-phase bus, it is important to consider the fault impedance. This impedance is zero for a bolted fault, equal to the arc impedance for an arcing fault, and represents the total fault impedance for a transmission-line insulator flashover. To derive sequence and phase currents, fault conditions are translated from the phase domain to the sequence domain.
For line-to-line faults occurring between phases B and C, the...
601

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関連する実験動画

Updated: May 3, 2026

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

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海洋変形断層に地震の滑り込み

R E Abercrombie1, G Ekström

  • 1Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, USA. rachel@seismology.harvard.edu

Nature
|March 10, 2001
PubMed
まとめ

海洋変形断層の滑り方は,地震の深さや断裂メカニズムを分析することによってよりよく理解できます. 以前報告された地震前のスロースリップ前駆者は,おそらくモデリングアーティファクトである.

科学分野:

  • 地球科学 地球科学 地球科学
  • 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:

  • 海洋変形断層は重要なプレート境界線ですが,その滑り方についてはほとんど理解されていません.
  • 以前の研究では,ゆっくりとした地震の断裂と,海洋変形地震に先立つ検出可能なゆっくりとした滑落が示唆されていた.
  • これらのプロセスを理解することは,地震の予測に影響を及ぼします.

研究 の 目的:

  • ロマンシュとチェーンの変形断層の地震の深さと破裂メカニズムを調査する.
  • 海洋石層における脆性破損の最大深さを決定する.
  • 1994年のロマンシェ地震とその潜在的な前駆者を再評価する.

主な方法:

  • 身体波のブロードバンド地震図をモデリングする.
  • ロマンシュ川とチェーンの14回の地震を分析して,断層を変換する.
  • 1994年のロマンシェ地震の源スペクトルの再計算.

主要な成果:

  • ロマンシュ変換の地震は,チェーン変換の地震よりも体系的に深い.
  • 海洋石層における脆性障害の最大深さは約600°Cである.

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

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The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults
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The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults

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関連する実験動画

Last Updated: May 3, 2026

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

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

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The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults
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The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults

Published on: November 6, 2021

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  • 1994年のロマンチェ地震の波波は,一つの断層の深い滑りによってよくモデル化されています.
  • 結論:

    • 以前報告された1994年のロマンシェ地震のスロースリップの前兆は,モデル不確実性の人工物である可能性が高い.
    • 地震の深さと断裂メカニズムは,海洋の変形断層の振る舞いに関する重要な洞察を提供します.
    • この研究は,海洋の石層における脆性障害の理解を洗練している.