当前位置: X-MOL 学术Sensors › 论文详情
Our official English website, www.x-mol.net, welcomes your feedback! (Note: you will need to create a separate account there.)
ime Distribution of Strong Seismic Events in the Fore-Sudetic Monocline in Context of Signals Registered by Water-Tube Gauges in Książ Geodynamic Laboratory
Sensors ( IF 3.9 ) Pub Date : 2021-02-25 , DOI: 10.3390/s21051603
Marek Kaczorowski , Damian Kasza , Ryszard Zdunek , Roman Wronowski

Changes in the stress field in Świebodzice Depression (ŚU) unit area are the reason of complex kinematics of the rock blocks consisting of rotations and horizontal/vertical displacements. The measurement system of the Geodynamic Laboratory in Książ, associated with rock blocks which are separated by faults, is a natural detector of tectonic activity. Installed in laboratory long water-tube gauges allowing to determine the functions of tectonic activity—TAF, and their derivatives. A comparison of the TAF with the seismic activity of the Fore-Sudetic Monocline showed that the strong seismic shocks (magnitude ≥3.6) occur in the Monocline only during defined and repeatable phases of the kinematic activity of the ŚU. Observed concordance proves the thesis of the existence of a large-scale, and largely homogeneous field of tectonic forces which, at the same time, cover the ŚU and the Fore-Sudetic Monocline units. The results of comparison between seismic events temporal distribution and phases of tectonic activity of the ŚU orogen indicate existence of the time relation between function of derivative of the tectonic activity (TAF) and seismic events.

中文翻译:

Książ地球动力学实验室中的水管测量仪记录的信号中,前南洋单斜线中强烈地震事件的动态分布

Świebodzice凹陷(ŚU)单位面积应力场的变化是岩石块运动学复杂的原因,其中包括旋转和水平/垂直位移。位于Ksiąthe的地球动力学实验室的测量系统,与被断层分开的岩石块相关,是构造活动的自然检测器。安装在实验室长水管仪表中,可以确定构造活动的功能— TAF及其衍生物。TAF与前南极单斜线的地震活动的比较表明,仅在theU的运动活动的确定的和可重复的阶段,强烈的地震冲击(震级≥3.6)发生在单斜线上。观察到的一致性证明了构造力的一个大范围,很大程度上均匀的存在的论点,同时覆盖ŚU和前单斜线单元。ŚU造山带地震事件的时间分布和构造活动的相位之间的比较结果表明,构造活动的导数函数(TAF)与地震事件之间存在时间关系。
更新日期:2021-02-25
down
wechat
bug