爱琴海地区GPS记录的20年同震位移数据库(1997-2017)及其与Mw和震源距离的标度

A. Ganas, Nikoletta Andritsou, Chrysanthi Kosma, P. Argyrakis, V. Tsironi, G. Drakatos
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引用次数: 6

摘要

我们描述并提供了1997-2017年期间希腊重大浅层地震的64个全球定位系统(GPS)位移数据点的数据集。地震地质学家、工程师和地震学家可以利用位移数据来更好地了解断层过程、破裂力学、地面运动模式,并在工程上应用。我们包括从近源到区域距离(2-132公里)的GNSS网络记录的11次全球CMT矩震级(Mw)在5.5和6.9之间的地震。我们还使用l1范数最小化回归对这些事件的峰值地面水平位移(PGD和PGD- s)的震级缩放特性进行了建模。我们的数据表明,在这个震级范围内,地震应变随距离几乎呈线性衰减。我们建立了一套基于PGD(单位厘米)和震源距离R(单位千米)的关系式,可用于近实时的快速估计地震震级。MwPGD = [LOG(PGD) + 8.2849]/(1.6810 - 0.2453LOG)MwPGD- s = [LOG(PGD) + 8.0839]/(1.6793 - 0.2447LOGR)
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A 20-yr database (1997-2017) of co-seismic displacements from GPS recordings in the Aegean area and their scaling with Mw and hypocentral distance
We describe and make available a dataset of 64 data points of Global Positioning System (GPS) displacements for significant, shallow earthquakes in Greece during the period 1997-2017. The displacement data can be used by earthquake geologists, engineers and seismologists in an effort to better understand the faulting process, the rupture mechanics, the pattern of ground-motions, and in engineering applications. We include recordings from GNSS networks at near-source to regional distances (2–132 km) for 11 earthquakes between global CMT moment magnitudes (Mw) 5.5 and 6.9. We also model the magnitude scaling properties of peak ground horizontal displacements (PGD and PGD-S) for these events using L1-norm minimisation regression. Our data indicate an almost linear attenuation of seismic strain with distance for this range of seismic magnitudes. We developed a set of relationships based on PGD (in cm) and distance to hypocentre R (in km), which may be used for the rapid estimation of the earthquake magnitude in near real-time.MwPGD = [LOG(PGD) + 8.2849]/(1.6810 – 0.2453LOGR)MwPGD-S = [LOG(PGD-S) + 8.0839]/(1.6793 – 0.2447LOGR)
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