Science. 1986 Sep 5;233(4768):1071-3. doi: 10.1126/science.233.4768.1071.
Coastal uplift associated with the great Mexican earthquake of 19 September 1985 and its principal aftershock produced widespread mortality of intertidal organisms along the coast of the states of Michoacán and Guerrero, Mexico. Measurements of the vertical extent of mortality at ten sites provided estimates of the magnitude of the vertical component of deformation along the coast. Within the affected area, uplift ranged from about 12 centimeters to about 1 meter, and no subsidence was observed. The observations are consistent with models of the tectonic deformation that results from buried slip on a shallow-dipping underthrust fault.
1985 年 9 月 19 日墨西哥大地震及其主要余震导致墨西哥米却肯州和格雷罗州沿海地区潮间带生物大量死亡。在十个地点测量的死亡垂直范围提供了沿海地区变形垂直分量大小的估计值。在受影响地区,隆起幅度约为 12 厘米至 1 米,没有观测到沉降。这些观测结果与浅层隐伏逆冲断层上的埋藏滑动导致的构造变形模型是一致的。