【摘要】 根据先前相似模型实验的结果 ,在板块边界驱动下 ,沿岩石圈下层 (含下地壳和岩石圈地幔 )传播的塑性流动波包括“快波”和“慢波” ,二者均属于黏性重力波 ,并分别由主波和辅波叠加而成。“快波”以 10 0 ～ 10 2 km/a量级的速度传播 ,已为塑性流动波控制下地震迁移的研究所证实。文中根据 7级以上强震的条带状分布图像 ,证明在喜马拉雅弧驱动下还存在着波速仅为 10 0 ～ 10 1m/a量级的“慢波” ,其中对 7级以上强震起控制作用的主要是“慢波”的辅波 ,其平均波长为 4 45km ,波速为 0 81～ 2 80m/a ,周期为 0 .16～ 0 .5 5Ma。“慢波”的边界起波时间距今约 1.34～ 4 .6 6Ma ,相当于上新世中期至早更新世中期 ,与喜马拉雅构造运动的主要活跃期 (幕 )之一相吻合。以喜马拉雅弧西段和东段为波源所形成的2个“慢波”系统的波峰带相互重叠 ,为 7级以上强震的发生提供了必要的能量背景更多还原

【Abstract】 The results inferred from the experiments of analogue modeling carried out previously have shown that two types of plastic-flow waves, "fast-wave" and "slow-wave", are induced in the lower lithosphere (including the lower crust and lithospheric mantle) under the driving at plate boundary; and both of them are the viscous gravity waves formed by the superposition of major and subsidiary waves. The major one is similar to solitary wave and the subsidiary one is traveling wave. The plastic-flow waves in the lower lithosphere control the seismic activities in the overlying seismogenic layer and result in the distribution of earthquakes along the wave-crest belts. The "fast-waves" propagated with velocities in the orders of magnitude of 10 0～10 2km/yr have been verified by the wave-controlled earthquake migration, showing the "decade waves" and "century waves" with the average periods of 10.8 and 93.4yr, respectively, which are originated from the Himalayan driving boundary. According to the recognition of the patterns of the belt-like distribution of strong earthquakes with M S≥7.0, it is indicated further in this paper that the "slow-waves" with velocities in the orders of magnitude of 10 0～10 1m/yr are also originated under the compression from the Himalayan driving boundary. The strong earthquakes with M S≥7.0 are controlled mainly by the subsidiary waves, because the major waves with the duration up to 10 6yr for each perturbation are impossible to result in the accumulation of energy enough for generating strong earthquakes owing to the relaxation of the upper crust. The subsidiary waves propagate with an average wave length of 445km and, as estimated in term of the requirement of elastic energy for strong earthquakes in the crust (the constraint of energy for strong earthquakes) and the actual situation of the apparently immobile wave-crest belts (the constraint of the relative immobility of wave-crest belts), with velocities of 0.81～2.80m/yr and periods of 0.16～0.55Ma. The wave-generating time at the Himalayan driving boundary is about 1.34～4.66Ma BP for the "slow-waves", corresponding to the stage from Mid Pliocene to Mid Early-Pleistocene and being identical with one of the major tectonic episodes of the Himalayan tectonic movement. It is shown from the recognition of the wave-controlled belts of strong earthquakes that two optimal patterns of wave-crest belts are originated simultaneously from the eastern and western segment of the Himalayan arc, respectively. The overlap of wave-crest belts of these two systems are responsible for the relative concentration of energy and the formation of the seismic-energy-background zones for strong earthquakes with M S≥7.0.更多还原