随后中—晚侏罗世时盆地南部沉降—沉积强度显示出变弱的趋势，期间没有再出现沉降—沉积再加强的现象。
Afterwards, the subsidence-sedimentation process slowed down gradually in the south of the Hefei Basin in the Middle-Late Jurassic without any strengthening phenomenon.
晚三迭世的近南北向构造和4）中侏罗世以来的整体掀斜构造。
The north-south structure in upper triassic epoch and, 4) The whole tilting structure after middle jurassic epoch.
早—中侏罗世研究区处于一种张扭构造环境之中，晚侏罗世盆地发生明显抬升和反转。
The study area was in a tectonic setting of transtension during Early and Middle Jurassic, and the basins were reversed and uplifted in Late Jurassic.
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