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Present Kinematic Regime and Recent Seismicity of Gulf Suez, Egypt

机译:埃及苏伊士湾的当前运动状态和最近的地震活动

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In this study we computed recent seismicity and present kinematic regime in the northern and middle zones of Gulf of Suez as inferred from moment tensor settlings and focal mechanism of local earthquakes that happened in this region. On 18 and 22 of July, 2014 two moderate size earthquakes of local magnitudes 4.2 and 4.1 struck the northern zone of Gulf of Suez near Suez City. These events are instrumentally recorded by Egyptian National Seismic Network (ENSN). The earthquakes have been felt at Suez City and greater Cairo metropolitan zone while no losses were reported. The source mechanism and source parameters of the calculated events were considered by the near-source waveform data listed at very broadband stations of ENSN and supported by the P-wave polarity data of short period stations. The new settling method and software used deem the action of the source time function, which has been ignored in most of the program series of the moment tensor settling analysis with near source seismograms. The obtained results from settling technique indicate that the estimated seismic moments of both earthquakes are 0.6621E + 15 and 0.4447E + 15 Nm conforming to a moment magnitude Mw 3.8 and 3.7 respectively. The fault plan settlings obtained from both settling technique and polarity of first-arrival indicate the dominance of normal faulting. We also evaluated the stress field in north and middle zones of Gulf of Suez using a multiple inverse method. The prime strain axis shows that the deformation is taken up mainly as stretching in the E-W and NE-SW direction.
机译:在这项研究中,我们计算了苏伊士湾北部和中部地区的近期地震活动性和当前的运动状态,这是根据该地区发生的弯矩张量沉降和局部地震的震源机制得出的。 2014年7月18日至22日,苏伊士湾北部地区靠近苏伊士城的地方发生了两次中度大小为4.2和4.1的中等地震。这些事件由埃及国家地震台网(ENSN)记录。在苏伊士市和开罗大都市区都感觉到了地震,但没有发生损失。 ENSN甚宽带站列出的近源波形数据考虑了计算事件的源机制和源参数,短周期站的P波极性数据支持了该数据。新的沉降方法和软件使用了源时间函数的作用,而在带有近源地震图的矩张量沉降分析的大多数程序系列中,这一点已被忽略。从沉降技术获得的结果表明,两次地震的估计地震矩分别为0.6621E + 15和0.4447E + 15 Nm,分别符合矩量Mw 3.8和3.7。从沉降技术和首次到达极性获得的故障计划沉降表明了正常故障的优势。我们还使用多重反演方法评估了苏伊士湾北部和中部地区的应力场。原始应变轴表明,变形主要是沿E-W和NE-SW方向的拉伸来吸收的。

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