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
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