更新阿卡巴湾的地震构造环境
Mona Abdelazim1, Mohamed N ElGabry2, Mohamed M Gobashy3
1Egyptian National Data Center (ENDC), National Research Institute of Astronomy and Geophysics (NRIAG), Helwan, Egypt. m.abdallah@nriag.sci.eg.
Scientific reports
|July 19, 2023
概括
阿卡巴湾的地震活动显示出明显的构造应力模式. 伊拉特盆地显示罢工滑动断层,而达喀尔盆地显示延伸,两者都存在于阿拉贡盆地.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地震学 地震学
背景情况:
- 阿卡巴湾是中东的一个地震活跃地区.
- 了解构造压力制度对于地震危险评估至关重要.
研究的目的:
- 确定阿卡巴湾 (包括伊拉特,阿拉贡和达喀尔盆地) 的压力状态.
- 分析地震数据以了解该地区的故障机制.
主要方法:
- 在113次地震 (2.5-7.2级) 中应用了反转技术.
- 分析了基于构造学区域化的地震数据子集.
主要成果:
- 确定了两个活跃的压力模式:埃拉特盆地中的罢工滑动和达喀尔盆地的延伸.
- 在阿拉贡盆地观察到罢工和扩展制度的共存.
- 最小的主力压力表明ENE趋势,几乎横向跨盆地延伸.
结论:
- 艾拉特盆地的压力模式与死海转变断层保持一致.
- 达卡尔盆地的延伸状态与红海北部的应力场相一致.
- 阿拉贡盆地的复杂压力很可能是由于相邻的构造体制的叠加.
相关概念视频
Effect of Sea Water on Concrete
291
Concrete exposed to seawater can undergo degradation like the dissolution of ettringite and gypsum, increasing the material's porosity and decreasing its strength. In contrast, the crystallization of salts within the concrete's pores can cause expansion, particularly above the waterline where evaporation occurs. Nonetheless, this expansion only happens when seawater, enabled by the concrete's permeability, manages to infiltrate the structure.
Concrete in areas between tide marks,...
Concrete in areas between tide marks,...
291
Electrostatic Boundary Conditions
515
Consider an external electric field propagating through a homogeneous medium. When the electric field crosses the surface boundary of the medium, it undergoes a discontinuity. The electric field can be resolved into normal and tangential components. The amount by which the field changes at any boundary is given by the difference between the field components above and below the surface boundary.
The surface integral of an electric field is given by Gauss's law in integral form and is related to...
The surface integral of an electric field is given by Gauss's law in integral form and is related to...
515
Magnetostatic Boundary Conditions
1.0K
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...
1.0K
Geoid and Ellipsoid
71
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...
71
Azimuths and Bearings
159
Azimuths and bearings are essential concepts in surveying, providing methods to express the direction of a line relative to a meridian. Azimuths refer to the clockwise angle measured from the north end of a reference meridian to the given line, ranging from zero to 360 degrees. This method gives a comprehensive directional reference within a full 360-degree circle, making it a straightforward way to communicate direction in various fields, including navigation, cartography, and...
159
Setting Time of Cement
202
The setting time of cement refers to the process of cement paste transitioning from a plastic state to a solid state. This process is crucial in construction as it dictates the timeframe for concrete placement, compaction, and finishing. The onset of this solidification is termed the initial set, indicating when the paste becomes unworkable. The final set is when the paste has solidified completely, and further handling or manipulation can no longer affect its shape. The cement strength is...
202


