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关于地下断层封闭性的讨论——以东营凹陷为例

王志欣 信荃麟   

  1. 石油大学
  • 收稿日期:1997-09-20 修回日期:1997-09-20 出版日期:1997-09-20 发布日期:1997-09-20

DISCUSSION ON THE SEALING PROPERTY OF DEEPLY BURIED FAULTS

Wang Zhi-xin, Xin Quan-lin   

  1. University of Petroleum, Beijing 100083
  • Received:1997-09-20 Revised:1997-09-20 Online:1997-09-20 Published:1997-09-20

摘要: 本文回顾并分析了前人进行断层封闭性评价的一些基本思路,并根据孔隙压力和有效应力原理提出了断层封闭性评价的新见解,断面的力学性质取决于该断面上有效直应力和剪应力的大小和方向;有效直应力为压性,则断面为封闭的,有效直应力的性质受控于有效地应力,而有效地应力的大小与流体压力密切相关;以前对断层封闭性的评价中所考虑的影响因素是不全面的,完全忽略了流体压力对断层封闭性的影响;断层封闭性不但是变化的,而且其变化是一种瞬时的、多次所复的过程;在探埋藏条件下,断层一般是封闭的。自然界中至少存在着两种引起地层压力快速上升并导致深部断层开启的机制:一是地震触发高压致裂;二是深部流体注入引最的连锁压裂。

Abstract: Sealing ability of faults is the key which controls the migration and accumulation of oil and gas along fault. In this paper, the authors reviewed and analyzed the fundamental ideas, in the prevailing evaluation of fault sealing property, and some new thinking about this work was made on the basis of the theory of effective stress. (1) The mechanical properties of a fault plane depends on the magnitude and direction of normal and shear stresses on that plane; compressive normal stress suggests that the fault plane is sealed: the nature of normal stress depends on the effective ground stress,which is otherwise closely related with formation pore pressure. (2)The prevailing evaluation of fault sealing property which completely neglected the influences of formation fluid pressure is not perfect; the fault sealing property has been changing for all the history in an instant, repeatful and eventful way. (3)Under deep burial, nearly all faults are generally sealed in relatively peaceful tectonic background. (4)In nature, there are at least two mechanisms which have repeatedly resulted in the natural fracturing of confined aquifers by high pressure: the first is “high pressure fracturing triggered by earthquakes”, i.e. the instant changes of geostress field during earthquakes can result in entremely high formation pressure which will further result in the opening of formerly sealed faults and subtle fractures; the other mechanism is “high pressure chain fracturing due to upward intrusion of deeply seated fluids.”