Average thrust and strike slip rate of Liangdang-Jiangluo fault is determined.
The slip rates of faults on the western QL mountains are around 1 mm/a or lower.
The decadal GPS velocity suggests that WQL is experiencing slow motions.
The NWW-trending faults of the WQL played a role in deformation transformation.
The slip rate of EKLF is not transferred to the WQLF or further north.