摘要
在“DSF”理论的基础上,本文将压缩观测水层的构造应力增量扩展成是时间任意函数的持续力情况,用这种持续力压缩水层产生喷涌的机理更具有普遍意义,而以单一矩形力为基础的成因理论,仅仅是持续力情况下的一个特例。本文介绍的就是这种扩展的“DSF”理论(The Extend Deformation Seepage Flow Theory)。本文还就扩展的“DSF”理论的意义等进行了讨论。
On the basis of the 'DSFM theory, this paper extends the concept of the tectonic stress increment compressing the observed aquifer into the condition of continupus force which is the arbitrary funcion of time. The mechanism of the gushing caused by compressing the aquifer with continuous force bears a much general significance, while the formation theory based on a single rectangular force is only a special example under the circumstances of continuous force. In this paper, we will introdue this ''extended deformation seepage flow' theory, which is regaded as the generalized DSF theory. We will also discuss the significance of this extended DSF theory at the end of the paper.
出处
《地震研究》
CSCD
北大核心
1989年第2期169-181,共13页
Journal of Seismological Research