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滦河中下游水系和新构造应力场
RIVER SYSTEM OF MIDDLE-LOWER REACHES OF LUANHE RIVER AND NEOTECTONIC STRESS FIELD
【摘要】 新构造应力场对地震形成机制、滑坡、水陆交通规划和水利工程布置都有重要的实用意义。本文根据沙氏法(A.E.Scheidegger)对滦河尤其是中下游水系格局进行了统计分析,并和土层节理、地震裂缝、地震断层面解等得出的区域构造应力场相互验证,从而得出了唐山近区的新构造应力场:最大压应力轴P1=70°~80° P2=50°最大张应力轴T1=340° T2=320°
【Abstract】 Neotectonic stress field is practically significant for mechanism of earthquake formation, landslide; water-land communication plans and irrigation works layout. According to A.E. Scheidegger’s method, this paper statistically analyses the layout of river system of the middle-lower reaches of Luanhe river especially. Based on joints of earth-layer, earthquake fissure and fault plane solution, the regional stress field is obtained. The field and the analysed result check each other, which speculates upon the neotectonic stress field in adjacent areas near Tangshan.Maximum principal compressive stress axes. P1=70°-80°, P2 = 50°: Maximum Principal tensile stress axes; T1=340°, T2 = 320°
- 【文献出处】 地震研究 ,Journal of Seismological Research , 编辑部邮箱 ,1989年01期
- 【被引频次】8
- 【下载频次】64