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The stress field of Vrancea region from fault plane solution (FPS)

机译:断裂平面解(FPS)从Vrancea区域产生的应力场

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摘要

The fault plane solutions (FPS) of 247 seismic events were used for stress field investigation of the region. The eigenvectors t,p,b, and moment tensor M components for each FPS were defined and computed numerically. The obtained results confirm the hypothesis of subduction-type intermediate depth earthquakes for the Vrancea seismic region and this may be considered the first approximation of the stress field for the whole of the Vrancea (intermediate depth) region.
机译:247个地震事件的断层平面解(FPS)用于该区域的应力场研究。每个FPS的特征向量t,p,b和矩张量M分量均已定义并进行了数值计算。获得的结果证实了Vrancea地震带俯冲型中深度地震的假设,这可以认为是整个Vrancea(中间深度)区域应力场的第一近似值。

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