Science. 1980 Mar 14;207(4436):1211-3. doi: 10.1126/science.207.4436.1211.
Aftershocks of the 29 November 1978 Oaxaca, Mexico, earthquake (surface-wave magnitude Ms = 7.8) define a rupture area of about 6000 square kilometers along the boundary of the Cocos sea-plate subduction. This area had not ruptured in a large (Ms >/= 7), shallow earthquake since the years 1928 and 1931 and had been designated a seismic "gap." The region has also been seismically quiet for small to moderate (M >/= 4), shallow (depth </= 60 kilometers) earthquakes since 1966; this quiet zone became about six times larger in 1973. A major earthquake (Ms = 7.5 +/- 0.25) was forecast at this location on the basis of the quiescence that began in 1973. The aftershock data indicate that an area approximately equivalent in size to the seismic gap has now broken.
1978 年 11 月 29 日墨西哥瓦哈卡地震(面波震级 Ms=7.8)的余震,沿着科科斯海板块俯冲带界定了一个约 6000 平方公里的破裂区。自 1928 年和 1931 年以来,这个区域没有发生过大规模(Ms≥7)、浅层地震,被指定为地震“空白区”。自 1966 年以来,该地区也一直没有小型到中型(M≥4)、浅层(深度≤60 公里)地震的活动;1973 年,这个安静区扩大了约 6 倍。根据 1973 年开始的平静,在此处预测到将发生一次大型地震(Ms=7.5±0.25)。余震数据表明,现在已经有一个大小大致相当于地震空白区的区域发生破裂。