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地下流体在地震孕育与发生中的作用——以张家口南部地热活动区为例
Effect of ground fluid in the earthquake preparation and occurrence——taking geothermal area in the southern Zhangjiakou as an example
【摘要】 对张家口南部地热活动区的水热活动特征及地震活动性进行了研究 ,结果表明 ,由于地下流体对断裂及其围岩的化学、物理作用 ,使断裂强度降低 ,而且随着流体温度的增高 ,循环深度的加深 ,这种作用将愈加强烈。表明地下流体在地震的孕育和发生中起着显著的作用。
【Abstract】 The characteristics of hydrothermal activity and earthquake activity in the southern Zhangjiakou are studied. The result indicates that the faulting strength will reduce owing to the effect of chemical and physical act of ground fluid on fault and its surrounding rocks, and this effect will be intenser with the increase of temperature and circulation depth of the fluid. It is suggested that the underground fluid will play a great role in the earthquake preparation and occurrence.
【关键词】 地下流体;
地震活动性;
循环深度;
水-岩作用;
【Key words】 Ground fluid; Earthquake activity; Circulation depth; Water rock interaction;
【Key words】 Ground fluid; Earthquake activity; Circulation depth; Water rock interaction;
【基金】 地震科学联合基金资助!(950 74 33)
- 【文献出处】 地震 ,EARTHQUAKE , 编辑部邮箱 ,2000年S1期
- 【分类号】P315.72
- 【被引频次】11
- 【下载频次】139