アラスカ州ウランゲル山で,スマトラ地震の後に定期的に発生した地震
Michael West1, John J Sánchez, Stephen R McNutt
1Alaska Volcano Observatory, Geophysical Institute, University of Alaska, Fairbanks, AK 99775, USA. west@gi.alaska.edu
まとめ
遠くの地震からの地表波は,ワレンゲル山の近くで局所的な地震を引き起こした. この地震の群れはレイリー波の地面運動と相関して発生し,通常の断層の単純な剪定障害を示唆しています.
科学分野:
- 地震学 地震学とは
- 地質物理学 地質物理学とは地質物理学です.
- テクトニクス (地質学) とは
背景:
- 2004年のスマトラ地震は,強力な地表波を生成しました.
- ワレンゲル山の近くの地震ステーションは,重要なデータを提供した.
研究 の 目的:
- 遠い地表波による局所地震の誘発を調査する.
- 表面波の動きと地元の地震活動との関係を理解する.
主な方法:
- ワレンゲル山からの地震データの分析.
- 地元の地震の発生とレイリー波の移動の相関.
- 横の伸縮張力の計算. 縦の伸縮張力の計算. 横の伸縮張力の計算.
主要な成果:
- ワレンゲル山 (Mount Wrangell) の近くで,14の局所的な出来事からなる11分間の地震群が引き起こされました.
- 地震はレイリー波の正の垂直地位移の相合に発生した.
- レイリー波の動きは,25キロパスカルまでの水平拡張性ストレスを示した.
結論:
- 遠い地表波は,局所的な地震を引き起こす可能性があります.
- トリガーメカニズムは,通常の故障での単純なシール故障を含みます.
- 観測により,大規模な地震が地域構造に及ぼす影響が明らかになった.
関連する概念動画
Modes of Standing Waves - I
A close look at earthquakes provides evidence for the conditions appropriate for resonance, standing waves, and constructive and destructive interference. A building may vibrate for several seconds with a driving frequency matching the building's natural frequency of vibration; this produces a resonance that results in one building collapsing while the neighboring buildings do not. Often, buildings of a certain height are devastated, while other taller buildings remain intact. This phenomenon...
Measuring Acceleration Due to Gravity
Consider a coffee mug hanging on a hook in a pantry. If the mug gets knocked, it oscillates back and forth like a pendulum until the oscillations die out.
A simple pendulum can be described as a point mass and a string. Meanwhile, a physical pendulum is any object whose oscillations are similar to a simple pendulum, but cannot be modeled as a point mass on a string because its mass is distributed over a larger area. The behavior of a physical pendulum can be modeled using the principles of...
A simple pendulum can be described as a point mass and a string. Meanwhile, a physical pendulum is any object whose oscillations are similar to a simple pendulum, but cannot be modeled as a point mass on a string because its mass is distributed over a larger area. The behavior of a physical pendulum can be modeled using the principles of...
Types of Building Separation Joints
Building separation joints divide large or complex building structures into smaller, discrete units that can move independently. These joints are categorized into three types: volume-change joints, settlement joints, and seismic separation joints.
Volume-change joints address the effects of expansion and contraction due to temperature and moisture variations. They are strategically placed at discontinuities in a building's mass where cracking is most likely and are spaced about 150 to 200 feet...
Volume-change joints address the effects of expansion and contraction due to temperature and moisture variations. They are strategically placed at discontinuities in a building's mass where cracking is most likely and are spaced about 150 to 200 feet...
Unsoundness of Aggregate due to Volume Change
Unsoundness in aggregates due to volume changes is primarily caused by the physical alterations aggregates undergo, such as freezing and thawing, thermal changes, and wetting and drying. Unsound aggregates, when subjected to these changes, result in volume change upon disintegration. This, in turn, contributes to the deterioration of concrete, including scaling, pop-outs, and cracking. Particular types of aggregates, such as porous flints, cherts, and those containing clay minerals, are...
Alkali Aggregate Reaction in Concrete
The alkali-aggregate reaction in concrete involves natural siliceous minerals in aggregates reacting with alkaline hydroxides derived from cement alkalis. This reaction forms an alkali-silica gel that absorbs water, swells, and increases in volume, which is confined by the surrounding cement paste, creating internal pressures that crack and disrupt the concrete. The extent of expansion and damage can be partly attributed to the alkali-silica reaction's osmotic hydraulic pressure and the...
Geoid and Ellipsoid
The Earth's shape is best described as an ellipsoid, a slightly flattened sphere created by rotating an ellipse around its minor axis. This flattening results in the polar axis being about 21 kilometers shorter than the equatorial axis. In contrast, the geoid represents the Earth's gravitational shape and aligns with the mean sea level (MSL). The geoid is an irregular equipotential surface where gravity is perpendicular at every point. Variations in Earth's mass distribution cause geoid...


