梁国平, 丁健民. 冀中平原深井水力压裂应力测量[J]. 华北地震科学, 1986, 4(4): 23-30.
引用本文: 梁国平, 丁健民. 冀中平原深井水力压裂应力测量[J]. 华北地震科学, 1986, 4(4): 23-30.
Liang Guoping, Ding Jianmin. HYDROFRACTURING STRESS MEASUR MENT IN DEEP WELL IN CENTRAL HEBEI PLAIN[J]. North China Earthquake Sciences, 1986, 4(4): 23-30.
Citation: Liang Guoping, Ding Jianmin. HYDROFRACTURING STRESS MEASUR MENT IN DEEP WELL IN CENTRAL HEBEI PLAIN[J]. North China Earthquake Sciences, 1986, 4(4): 23-30.

冀中平原深井水力压裂应力测量

HYDROFRACTURING STRESS MEASUR MENT IN DEEP WELL IN CENTRAL HEBEI PLAIN

  • 摘要: 本文叔述了在冀中平原油井水力压裂应力测量原理。通过该地区十口井油井的水力压裂应力测量结果表明,在1500~3200米深度范围内,三个主应力是随深度成线性增加的,它们之间的关系为:SH >SV >S。此外,根据在河北省易县的水力压裂应力测量和震源机制解结果,表明该地区的最大水平主应力方向为北东到北东东向。由此证明,冀中平原地区的现代地壳运动是以水平作用为主。同时还表明该地区的四组断裂的活动性质:NE和EW向断裂为引张类型,NNE向断裂为右旋走向滑动类型,NW向断裂为左旋走向滑动类型。

     

    Abstract: The principles of hydrofracturing stress measuremen in oil wells in the central Hebei plain have been given. The measurement results of ten oil wells in this region show that three principal stresses linearly increase with depth within 1500m-3200m;their relation is sh >SV >Sh. In addition according to the results of hydrofracturing stress measurement in Yixian county of Hebei province and focal mechanism, the direction of major horizontal principal stress is NE-NEE. it is shown that recent crustal movement in the central Hebei plain is mainly horizontal, and the active properties of the four groups of faults in the region are as following, NE and EW faults are tensile, NNE are right-lateral strike slip and NE are left-lateral strike slip.

     

/

返回文章
返回