东河砂岩是一套覆盖广泛的海侵初期的沉积产物，但不是一个等时沉积体，相当于晚泥盆世晚期至早石炭世早期沉积，具体沉积时间各地有差异。
The Donghe Sandstone was broadly deposited in the early stage of the marine transgression, but it is not an isochronous stratigraphic unit.
本文应用沉积体系的研究方法，恢复了福建省晚泥盆世-中侏罗世地层的古沉积面貌。
The Late Devonian-Middle Jurassic depositional systems in Fujian Province arereconstructed in the paper.
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