石炭系底部的东河砂岩是一套优质储集层和富油层，也是塔里木盆地的主要产油层。
The Donghe sandstones in the base of the Carboniferous was an excellent reservoir and main oil-producting interval in the Tarim Basin.
泥岩和砂岩、灰岩等软硬岩石之间的差异风化孕发了陡崖底部的岩腔，内部泥岩的应力风化加速了岩腔发育。
Different weathering velocities for sandstone, carbonite and mudstone triggered rock cells in mudstone below cliffs, weathering in stress status sped up the development of rock cells.
周围悬崖的地质损害导致了大块的砂岩堆积在其底部，对周边的沙滩环境造成了污染。
Erosion of the cliffs produces large blocks of sandstone that litter the beaches at the foot of the cliffs.
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