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相关概念视频

Travelling Waves01:04

Travelling Waves

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 water;...
Modes of Standing Waves - I01:03

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...
Relation Between the Distributed Load and Shear01:23

Relation Between the Distributed Load and Shear

Understanding the relationship between the distributed load and shear force in structural analysis is crucial for analyzing beams subjected to various loading conditions. Consider the case of a beam experiencing a distributed load, two concentrated loads, and a couple moment.
The Electrical Double Layer01:30

The Electrical Double Layer

In the region where two bulk phases meet, an intricate electric charge distribution arises due to charge transfer, ion adsorption, molecular orientation, and charge distortion. This complex distribution is commonly referred to as the electrical double layer.When a solid electrode interfaces with ions in an electrolyte solution, the speed of electron transfer dictates the rates of oxidation and reduction. The electrode acquires a charge through the escape of atoms into the solution as cations or...
Fault Types01:18

Fault Types

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...
Types of Building Separation Joints01:23

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...

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Conformation of Fibronectin Fibrils Varies: Discrete Globular Domains of Type III Repeats Detected.

Microscopy and microanalysis : the official journal of Microscopy Society of America, Microbeam Analysis Society, Microscopical Society of Canada·1999
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相关实验视频

Updated: Jul 7, 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

奇奇地震序列:在台湾发生了活跃的,异序的推力断层.

Kao1, Chen

  • 1Institute of Earth Sciences, Academia Sinica, Nankang, Taipei, Taiwan 115, Republic of China. Department of Geology and Mid-America Earthquake (MAE) Center, University of Illinois, Urbana, IL 61801, USA.

Science (New York, N.Y.)
|July 6, 2000
PubMed
概括

1999年的奇奇地震序列主要是由中度下降的推力断层产生的. 一个更深的地震区存在,这表明无地震基底脱落和正常断层.

科学领域:

  • 地震学 地震学
  • 构造学 构造学 构造学 构造学
  • 地质地质地质地质地质地

背景情况:

  • 1999年台湾的奇奇地震是一个主要的地震事件.
  • 了解导致断层结构对于地震危险评估至关重要.

研究的目的:

  • 为了确定导致1999年9月20日奇奇地震的占主导地位的断层结构.
  • 调查台湾中部的地下地质和地震区域.

主要方法:

  • 结合了来自40多个地震事件的精确焦点深度和断层平面解决方案.
  • 合成的地下地质数据.

主要成果:

  • 确定了一个主导的,适度下降的推力断层 (20-30度),产生远离变形前线的地震.
  • 在主推力下方大约15公里处发现了第二个亚平行地震区.
  • 观察到基底脱落和遗留正常断层似乎都是无地震的.

结论:

  • 确定的地震区域与台湾构造框架的先前模型有所不同.
  • 这项研究表明,无地震基底脱落和正常断层在该地区的地震构造学中发挥着作用.

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Last Updated: Jul 7, 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

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

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Evolution of Staircase Structures in Diffusive Convection
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Evolution of Staircase Structures in Diffusive Convection

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