根据昆仑山口西地震测线断层围陷波的观测结果，可推断该处破裂面宽度为300m左右，远远大于地表破裂带的宽度。
Based on the fault zone trapped waves observed in Kunlun Mountain Pass region, the width of the rupture plane is deduced to be about 300 m and is greater than that on the surface.
作为尝试，对昆仑山口西m(下标s) 8.1地震触发的北京地区断层活动进行了反演。
As an attempt, we inverse the assumingly active faults' slips triggered by the m (subscript s) 8.1 Kunlun Mountain earthquake over Beijing area.
根据昆仑山口西8.1级地震前后GPS测点的位移速率，用弹性模型公式计算了地壳应变参数。
Based on the velocities of GPS sites before and after the M8.1 Kunlunshan earthquake, the crustal strain parameters are calculated with the elastic model.
玛尼7.9级地震对昆仑山口西8.1级地震的触发作用及动力背景初探。
Study of Triggering Action Between Mani(M_S7.9) and Kunlun(M_S8.1) Great Earthquakes and Their Dynamic Background.
玛尼7.9级地震对昆仑山口西8.1级地震的触发作用及动力背景初探。
Study of Triggering Action Between Mani(M_S7.9) and Kunlun(M_S8.1) Great Earthquakes and Their Dynamic Background.
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