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Afterslip distribution following the 2003 Tokachi-oki earthquake: An estimation based on the Green's functions for an inhomogeneous elastic space with subsurface structure

机译:2003年十胜冈地震后的后滑分布:基于格林函数的地下结构非均匀弹性空间估计

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We derive the 1-yr afterslip distribution following the 2003 Tokachi-oki (Hokkaido, northeastern Japan) earthquake (M_w 8.0) by inverting geodetic data, i.e., horizontal and vertical displacements, at 142 land stations of the Global Positioning System (GPS) in Hokkaido and northernmost Tohoku districts, together with vertical displacements at two offshore stations of pressure gauge (PG) off the Pacific coast of Hokkaido. We use the Green's functions (GFs), calculated with a finite element method, for an inhomogeneous elastic (IE) model incorporating subsurface structure. Obtained results show a striking feature of the distribution pattern of significant afterslip, namely, a U-shaped afterslip zone encircling the co-seismic rupture zone of the 2003 event. Amounts of the 1-yr afterslip reach up to 0.9 m, and total seismic moments released from all afterslip zones are of the order of 1021 N m, corresponding to an earthquake of M_w 8.0. For comparison, we also estimate the 1-yr afterslips based on GFs for the homogeneous elastic (HE) model to find that the total seismic moment with GFs for the IE model is larger than that with GFs for the HE model by ~33% (when the most probable values are compared) if we assume a rigidity of 40 GPa. This result implies that inhomogeneities due to subsurface structure have an important role in geodetic inversions.
机译:我们通过倒转全球142个全球定位系统(GPS)上的大地测量数据(即水平和垂直位移),推导出2003年十胜冈(日本东北海道)地震(M_w 8.0)之后的1年后滑分布。北海道和最北部的东北地区,以及北海道太平洋沿岸的两个压力表(PG)的近海站的垂直位移。对于包含地下结构的非均匀弹性(IE)模型,我们使用通过有限元方法计算的格林函数(GF)。获得的结果显示出明显的余震分布模式的显着特征,即环绕2003年地震同震破裂带的U形余震带。 1年后滑移的量达到0.9 m,并且从所有后滑带释放的总地震矩约为1021 N m,对应于M_w 8.0级地震。为了进行比较,我们还基于均质弹性(HE)模型的GFs估计了1年后滑动,发现IE模型的GFs的总地震矩比HE模型的GFs的总地震矩大〜33%(比较最可能的值时),如果我们假设刚性为40 GPa。该结果表明,由于地下结构引起的不均匀性在大地测量反演中具有重要作用。

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