分析了1668 年山东郯城8?级大震区附近地壳深部结构特点，以天然地震走时层析成像得到的三维地壳速度结构，主要以中地壳低速层和莫霍面深度为依据，对34°～36°N，118°～119°E区间按经、纬度和斜向扫描，得到相应地壳速度剖面。对比结果，获得与该地震深部结构特点一致的区域，推测震中范围位于34.8°～35.2°N，118.2°～118.7°E，较合理的震中位于35.1°N，118.6°E，震源深度约20km。

The deep structure features around the Tancheng M8? earthquake in 1668 has been analyzed in the paper． On the basis of the crustal velocity structure of seismic traveltime tomography，especially the low velocity layer of middle crust and Moho depths，we scanned the deep velocity distribution in the area of 34° ～ 36°N，118° ～ 119°E along latitude，longitude and deflection direction，and located the area with the feature in agreement with the deep structure features around the Tancheng M8 earthquake in 1668． The location is 34. 8° N ～ 35. 2° N， 118. 2°E ～ 118. 7°E． The suitable location is 35. 1°N，118. 6°E with a depth of 20km．

国家自然科学基金( 40974031) ，江苏省科技发展项目( BE2009691) 资助