地震地质 ›› 2001, Vol. 23 ›› Issue (1): 49-54.

• 构造地质 • 上一篇    下一篇

延怀盆地上地壳热流体特征及其与地震活动的关系

车用太1, 王基华1, 鱼金子1, 刘五洲1, 宋贯一2   

  1. 1. 中国地震局地质研究所, 北京 100029;
    2. 河北省地震局, 石家庄 050021
  • 收稿日期:2000-06-30 修回日期:2000-10-31 出版日期:2001-03-07 发布日期:2009-10-26
  • 基金资助:
    地震科学联合基金(9507433)资助;中国地震局地质研究所论著2001B0004.

CHARACTER OF THERMAL FLUIDS IN UPPER CRUST AND RELATIONSHIP WITH SEISMICITY IN YANQING-HUAILAI BASIN

Che Yongtai1, Wang Jihua1, Yu Jinzi1, Liu Wuzhou1, Song Guanyi2   

  1. 1. Institute of Geology, China Seismological Bureau, Beijing 100029;
    2. Seismological Bureu of Hebei Province, Shijiazhuang 050021
  • Received:2000-06-30 Revised:2000-10-31 Online:2001-03-07 Published:2009-10-26

摘要: 系统研究了延怀盆地上地壳热流体的温度、水化学、气体化学与同位素化学特征,确定热水成因与大气降水渗入有关,并计算了热储温度与水循环深度,认为热水活动对中小地震活动有一定的控制作用并影响断裂活动强度。

关键词: 延怀盆地, 地壳流体, 地震活动, 断裂活动

Abstract: In this paper, some characters of temperature, hydro-chemistry, gas-chemistry and isotope chemistry of thermal fluids in upper crust of the Yanqing-Huailai basin are studied. The genesis of atmospheric water permeating of thermal fluids is determined. The temperature of thermal reservoir and circulation depth of thermal fluids are calculated. And their relationships with seismic and fault activity are discussed.

Key words: Yanqing-Huailai basin, Crust fluid, Seismicity, Fault activity