There is a gradient zone from the west to the east side of the fault zone,rising from an average of 55.35mW/m 2 on the west side to an average of 67.78mW/m 2 on the east side.

• 沿断裂带存在一条明显的热流梯度递变带，东侧平均热流值（67.；78mW/m2）明显高于西侧平均值（55