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应用中国数字地震台网（ＣＤＳＮ）记录的长周期体波波形数据，反演了１９８８年１１月６日中国云南省澜沧－耿马ＭＳ７．６地震的矩张量，求得了其震源机制和震源时间过程．反演结果表明，断层面解的一个节面是右旋走滑断层，另一个节面是左旋走滑断层；震源时间过程较简单，持续时间约１５ｓ；标量地震矩为６．４×１０２０Ｎ·ｍ．根据地质资料、区域构造、野外观测和余震震中分布，确认走向３１３°的节面是地震断层面，主压应力轴位于几乎水平的南北向
The long-period body-wave waveform data recorded by China Digital Seismograph Network (CDSN) were used to inverse the moment tensor of the Lancang-Gengma MS7.6 earthquake on November 6, 1988 in China. The focal mechanism and Source time course. The inversion results show that one nodal plane of the fault plane is a right-lateral strike-slip fault and the other nodal plane is a left-lateral strike-slip fault. The source time is relatively simple with a duration of about 15s. The scalar seismic moment is 6.4 × 1020N · m. Based on the geological data, regional tectonics, field observations and the epicentral distribution of aftershocks, it is confirmed that the section heading toward 313 ° is the seismic fault plane and the principal compressive stress axis is located in an almost horizontal north-south direction