威海市宝泉汤温泉成因及其对断裂和地震活动性的影响

杜桂林, 曹文海, 翟滨. 威海市宝泉汤温泉成因及其对断裂和地震活动性的影响[J]. 海洋地质与第四纪地质, 2012, 32(5): 67-72. doi: 10.3724/SP.J.1140.2012.05067
引用本文: 杜桂林, 曹文海, 翟滨. 威海市宝泉汤温泉成因及其对断裂和地震活动性的影响[J]. 海洋地质与第四纪地质, 2012, 32(5): 67-72. doi: 10.3724/SP.J.1140.2012.05067
DU Guilin, CAO Wenhai, ZHAI Bin. GENESIS OF BAOQUANTANG HOT SPRING IN WEIHAI AND ITS INFLUENCE ON FAULTING AND SEISMIC ACTIVITIES[J]. Marine Geology & Quaternary Geology, 2012, 32(5): 67-72. doi: 10.3724/SP.J.1140.2012.05067
Citation: DU Guilin, CAO Wenhai, ZHAI Bin. GENESIS OF BAOQUANTANG HOT SPRING IN WEIHAI AND ITS INFLUENCE ON FAULTING AND SEISMIC ACTIVITIES[J]. Marine Geology & Quaternary Geology, 2012, 32(5): 67-72. doi: 10.3724/SP.J.1140.2012.05067

威海市宝泉汤温泉成因及其对断裂和地震活动性的影响

  • 基金项目:

    威海市科技发展规划项目(2008GGA000003)

详细信息
    作者简介: 杜桂林(1981-),男,硕士生,主要从事地震地质、震害防御及GIS应用等工作,E-mail:duguilin2100@163.com
  • 中图分类号: P546

GENESIS OF BAOQUANTANG HOT SPRING IN WEIHAI AND ITS INFLUENCE ON FAULTING AND SEISMIC ACTIVITIES

  • 威海市是胶东地区温泉资源比较丰富的地区,而研究温泉与断裂及地震活动性的关系具有非常重要的意义。宝泉汤温泉位于市区的东部,是一种富含各种微量元素、矿化度较高的地热水,水化学分析表明,温泉水属于Cl-Na·Ca型;温泉受NW向神道口断裂和近EW向城南河断裂的控制,大气降水和海水顺着断层或断裂破碎带下渗和深循环形成温泉,地热水循环深度能达到2 022.14 m;温泉水循环对断裂及围岩有弱化作用,和温泉的热能释放作用一起降低了断裂和本区地震活动性。
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出版历程
收稿日期:  2012-06-13
修回日期:  2012-08-29

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