The results indicate that the uplift rates of the two sides of the Muping Ji mo fault zone of the past 124ka. are different. The uplift rate of the west side is about 0.50mm/a,while the that of the east side is only 0.15mm/a.

• 结果表明，12.；4万年以来牟平－即墨断裂带两侧的构造抬升速率有明显差异，断裂带西侧沿岸为0