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相关概念视频

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.
The difference between the true and apparent weights is proportional to the square of the Earth's...
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Forced Oscillations01:06

Forced Oscillations

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When an oscillator is forced with a periodic driving force, the motion may seem chaotic. The motions of such oscillators are known as transients. After the transients die out, the oscillator reaches a steady state, where the motion is periodic, and the displacement is determined.
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Normal Stress01:19

Normal Stress

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Normal stress is a type of stress that occurs when forces act perpendicular, or normal, to a material's cross-sectional area. This stress often arises in structures when subjected to axial loading, which is the application of force along the axis of an object. A practical example of this can be found in bridge truss members.
When a rod is under axial loading, the internal forces and corresponding stress are normal to the plane of the section, so it is termed normal stress. It's important to...
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Fault Types01:18

Fault Types

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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...
503
Vibrating Concrete01:19

Vibrating Concrete

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Mechanical vibrators are instrumental in compacting newly poured concrete within formwork and around reinforcements. This process is essential to eliminate trapped air pockets and establish a dense concrete mass. One widely used method is vibrating by internal vibrators, often referred to as a poker vibrator or immersion vibrator. It is rapidly inserted through the full depth of the freshly laid concrete and slightly extends into the layer below it (which remains in a plastic state). Consistent...
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Carbonation Shrinkage01:24

Carbonation Shrinkage

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Atmospheric CO2 penetrates the concrete's pores and, in the presence of moisture, forms carbonic acid, which then reacts with calcium hydroxide in the hydrated cement, forming calcium carbonate. This process reduces the concrete's volume and is termed carbonation shrinkage.
The concrete's permeability is slightly reduced as calcium carbonate produced during the reaction fills its pores. Furthermore, its strength is slightly enhanced as the water released during the reaction...
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相关实验视频

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

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在圣安德烈亚斯断层深处发生非火山性震动.

Robert M Nadeau1, David Dolenc

  • 1Berkeley Seismological Laboratory, 211 McCone Hall, University of California, Berkeley, CA 94720-4760, USA. nadeau@seismo.berkeley.edu

Science (New York, N.Y.)
|December 14, 2004
PubMed
概括

科学家们在加利福尼亚州圣安德烈亚斯断层深处发现了非火山震动活动. 这种发生在地震产生的区域以下的地震信号可能与当地地震模式相关.

科学领域:

  • *地震学和构造物理学:研究地震现象和板块边界动态.

背景情况:

  • *圣安德烈亚斯断层是加利福尼亚州的一个主要的变形板边界,与1857年特吉安堡地震等重大地震事件有关.
  • *地震活动,包括地震,主要被认为起源于地球地的地震带.

研究的目的:

  • * 识别和描述圣安德烈亚斯断层沿线的非火山震动活动.
  • * 确定这次地震的深度和潜在关系与当地的地震性.

主要方法:

  • *对地震数据的分析,以检测长时间的地震信号,缺乏明确的P或S波 (非火山震动).
  • * 在转变板边界区域内地理定位震动活动.

主要成果:

  • * 在20至40公里深处发现非火山震动活动.
  • * 这次地震发生在典型的地震带 (上方15公里) 以下.
  • *观察到震动活动率与当地地震活动变化之间的潜在相关性.

结论:

  • * 在圣安德烈亚斯断层深处,地震带以下,存在非火山性震动.
  • *这种深度地震活动可能在断层系统的更广泛的地震行为中发挥作用.

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