作为力矩张量反演伪影的表观非双耦合成分

Boris Rösler, Seth Stein, A. Ringler, Jiří Vackář
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引用次数: 0

摘要

对全球和区域目录中的地震力矩张量进行汇编后发现,非双偶(NDC)成分普遍存在,与双偶(DC)震源的平均偏差约为 20%。它们的分布仅随震级、断层机制或地质环境而略有不同。这种一致性表明,对于大多数地震,尤其是断裂过程较为简单的小地震,NDC成分在很大程度上是力矩张量反演程序的伪影。Mw<6.5的单个地震的NDC成分在不同地震序列之间只有微弱的相关性,这一事实也支持了这种可能性。我们通过使用一种地球模型生成全球地震双偶成分的合成地震图,并用另一种地球模型进行反演,来探索这种可能性。为了与不同地球模型的波形相匹配,反演改变了地震机制,加入了大量的 NDC 成分,同时在很大程度上保留了断层几何(DC 成分)。由此产生的 NDC 分量的大小和分布与全球中心力矩张量(GCMT)目录中报告的地震相似。数值实验复制了力矩张量目录中报告的普遍 NDC 分量的一般特征,这意味着这些分量在很大程度上是反演没有充分考虑横向变化的地球结构影响的产物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Apparent Non-Double-Couple Components as Artifacts of Moment Tensor Inversion
Compilations of earthquake moment tensors from global and regional catalogs find pervasive non-double-couple (NDC) componentswith a mean deviation from a double-couple (DC) source of around 20%. Their distributions vary only slightly with magnitude, faulting mechanism, or geologic environments. This consistency suggests thatfor most earthquakes, especially smaller ones whose rupture processes are expected to be simpler, the NDC components are largely artifacts of the moment tensor inversion procedure. This possibility is also supported by the fact that NDC components for individual earthquakes with Mw<6.5 are only weakly correlated betweencatalogs. We explore this possibility by generating synthetic seismograms for the double-couple components of earthquakes around theworld using one Earth model and inverting them with a different Earth model. To match the waveforms with a different Earth model, the inversion changes the mechanisms to include a substantial NDC component while largely preserving the fault geometry (DC component). The resulting NDC components have a size and distribution similar to those reported for the earthquakes in the Global Centroid Moment Tensor (GCMT) catalog. The fact that numerical experiments replicate general features of the pervasive NDC components reported in moment tensor catalogs implies that these components are largely artifacts of the inversions not adequately accounting for the effects of laterally varying Earth structure.
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